Dokument 1 - E-Dissertationen der UHH

Transcription

Benthic bacteria in the German Bight:
Characterising community structure and influencing
environmental factors
Dissertation
Zur Erlangung der Würde des Doktors der Naturwissenschaften
des Department Biologie, der Fakultät für Mathematik, Informatik und Naturwissenschaften,
der Universität Hamburg
vorgelegt von
Rebecca Störmer
Aus Iserlohn
Hamburg 2013
___________________________________________________________________
Center for Earth Systems
Research and Sustainability
Prof. PhD. Myron A. Peck
Institute of Hydrobiology and
Fisheries Science
An die/den Vorsitzende/n desPromotionsausschusses
des Departments Biologie über die Leitung des
Departments Biologie
Martin‐Luther‐King‐Platz 2
20146 Hamburg Olbersweg 24 • D‐22767 •
Hamburg
Tel +49 4042 838 6602
Fax +49 4042 838 6618
myron.peck@uni‐hamburg.de
Sehr geehrte Frau Vorsitzende/sehr geehrter Herr Vorsitzender,
The thesis by Frau Rebecca Störmer has been written in acceptable, scientific English.
hiermit bestätige ich dass die vorliegende Arbeit von Frau Störmer in korrektem Englisch verfasst wurde.
Mit freundlichen Grüßen
Prof. Myron A. Peck
Hamburg, 01.10.2012
CONTENT
GENERAL INTRODUCTION ............................................................................................................... 1
RESEARCH AIMS ............................................................................................................................. 9
OUTLINE .......................................................................................................................................... 11
CHAPTER I .......................................................................................................................................... 13
Biogeography of benthic bacterial communities in the German Bight ............................................. 13
CHAPTER II ......................................................................................................................................... 35
Impact of ocean dumping on bacterial communities ......................................................................... 35
I: Fine-scale investigations at a dumping site.................................................................................... 35
CHAPTER III ........................................................................................................................................ 61
Impact of ocean dumping on bacterial communities ......................................................................... 61
II: GeoChip-based analysis of bacterial communities at a dumping site........................................... 61
GENERAL DISCUSSION .................................................................................................................... 81
SUMMARY .......................................................................................................................................... 90
ZUSAMMENFASSUNG ...................................................................................................................... 92
REFERENCES ...................................................................................................................................... 94
DANKSAGUNG ................................................................................................................................. 108
GENERAL INTRODUCTION
__________________________________________________________________________________
Study area: North Sea
The greater North Sea is located on the continental shelf of north-west Europe and can be
divided into the shallow southern North Sea (depths on average < 40 metres), the central
North Sea, the Norwegian Trench and the Skagerrak (OSPAR 2000). The average
temperature ranges between 6°C in winter and 17°C in summer, while salinity is varying
between 15 – 25 in estuaries and 32 - 35 in northern areas (OSPAR 2000). The seafloor
topography of the North Sea is dominated by an ancient, north-south orientated continental
drift depression. This depression is covered by terriginous sediment deposits, several
kilometres thick, which consist mainly of sand and sandy silt (OSPAR 2000). Water
movement in the North Sea is predominantly influenced by tidal, current and storm events as
well as density gradients resulting from freshwater input (Howarth 2001). These motions are
too weak to affect sediments characteristics in the central or northern North Sea. Contrary, in
the shallow southern part of the North Sea, remarkable sediment transport processes occur.
Principally, fine-grained material is transported over a considerable distance into deeper areas.
Another source of sediment transports are estuaries along the coast. These transports are
widely depending on estuary gradients and fluctuate according to tidal and seasonal changes
(OSPAR 2000).
Estuarine gradients
The river runoff in estuaries determines the deposition of sediments but also of nutrients
(Atlas and Bartha 1987). Estuaries represent therefore highly productive areas. These regions
are characterised by a multitude of environmental gradients. The mixing of freshwater and
marine waters implies salinity and temperature gradients. Furthermore pH and organic
loading fluctuate on tidal and seasonal ranges. Living in this highly variable environment
requires adaptations and eurytolerance to many environmental factors such as salinity,
temperature or pH variations (Atlas and Bartha 1987).
The German Bight is situated in the southern part of the North Sea, predominantly influenced
by the discharges of Elbe and Weser Rivers (Hickel et al 1993). This region represents
probably the most eutrophied area in the North Sea. Due to the residual counter clockwise
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currents and the positioning of estuaries intense accumulations of eutrophying substances
occur (Hickel et al 1993). Studies conducted in the past 50 years in the German Bight were
addressing
mainly
eutrophication
(Hickel
et
al
1993,
Rachor
1990),
pollution
(Bester et al 1998, Gee et al 1992, Schwarzbauer et al 2000, Vauk and Schrey 1987) and
storm surges (Woth et al 2006). Long term studies suggest changes of the hydrographic
regime and biota around Helgoland coupled with increasing temperature (on average 1.67°C)
and salinity (Wiltshire et al 2010). Hence, it becomes obvious, that the German Bight
represents a highly anthropogenic influenced and variable ecosystem. On top of that, other
anthropogenic activities as fishery, industry, shipping and the maintenance of coastal rivers
and ports are affecting this region.
Anthropogenic perturbation in the North Sea
Human interventions in the marine ecosystem are manifold. Coastal areas are impacted by
riverine input of contaminants and nutrients originating from industry, urbanisation and
agriculture (Boetius et al 2000, Burak et al 2004, Witt and Trost 1999). Intensive fishing
industry harms not only fish stocks but also the benthos by fishing practices such as trawling
(Freese et al 1999). At the coastline, dredging procedures are possibly changing
hydrodynamics in estuaries (Bale et al 2007). On the sea global shipping causes litter input,
oil contamination and ballast water release (Balas et al 2006, Gundlach and Hayes 1978).
Another issue of great concern represents waste disposal at sea. Different kinds of waste as
for instance low-level radioactive waste (Phillips et al 2011), sewage sludge and dredged
sediment resulting from maintenance of navigation channels and port facilities (OSPAR 2009,
Stronkhorst et al 2003) are deposited at sea. The impacts of these human induced
perturbations are extensively studied but focus predominantly on higher organisms
(Gee et al 1992, Mühlenhardt-Siegel 1981, Vauk 1984, Vethaak et al 1992).
Dumping activities in the German Bight
The history of dumping activities in the German Bight goes back to the 1960s. 20 000 m³ of
sewage sludge from the city of Hamburg was dumped monthly into the eastern German Bight
(Mühlenhardt-Siegel 1981). A reported decline in macrozoobenthic species richness led to a
cessation of the dumping activities. Recently, in 2005, the city of Hamburg received
permission to dump lowly polluted sediments in the same area (HPA 2005) and the dumping
activities were resumed. Hence, in between the years 2005 and 2010 approximately
6 000 00 cubic metres sediment were removed from the Elbe River near the port area of
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Hamburg and dumped at the prescribed site. The dumping activity is accompanied by an
elaborate monitoring program. Twice a year samples from 125 stations at the dumping and a
reference site were taken in order to estimate the effect of the dumping activity. Bearing at the
disposal site revealed that a main proportion of the sandy material forms a three meters high
rising at the dumping centre. Fine-grained fractions were tracked with Acoustic Doppler
Current Profiler (ADCP) recording that fine-grained material is transported up to eight
kilometres until it reaches the seafloor (HPA 2005). In order to elucidate the impact of the
dumping activity on the environment, contaminant content, macrozoobenthos and fish fauna
data were recorded. Comparing measurements before and along the dumping activities
revealed a significant increase in heavy metals, namely mercury, cadmium and zinc as well as
organic pollutants, precisely poly aromatic hydrocarbons and organotin compounds. At the
same time species richness and density of the macrozoobenthos decreased (HPA 2010). So
far, bacterial community analyses have not been included in the monitoring program. To
implement this ecologically important group of organisms, we started an interdisciplinary
project in 2009 with the Hamburg Port Authority, in charge for the monitoring, the
environmental agencies of Schleswig-Holstein and Lower Saxony and the Federal Institute of
Hydrology (BfG). This pilot study aimed to analyse the bacterial community with respect to
the dumping activities and to examine the potential of bacterial community analyses to serve
as a proxy for environmental perturbation. Participating in three monitoring campaigns,
samples for community and functional structure of benthic bacteria were collected.
Bacteria in marine sediments
Marine sediments cover more than 70 % of the Earth’s surface. Their physical and chemical
conditions are unique in many ways. Grain size distributions are their most important physical
characteristic (Sommer 2005). Typically, sediment is divided by its grain size into six
fractions: < 4µm defined as clay, 4 – 63 µm defined as silt, three sand fractions and gravel
(2 - 6 mm). The composition of these grain size fractions determines the distribution of
physicochemical factors such as water or oxygen penetration. Both depend on the sediment
porosity. The different sediment types offer further conditions: organic substances form
aggregates in muddy sediments (containing a high proportion of silt and clay) and are more
available to microorganisms than in sandy sediments (Sommer 2005). Contrary, sandy
sediments are much looser than muddy sediments and allow a deeper water and oxygen
penetration. In any case, the oxygen penetration stops at a certain depths. The abrupt lack of
oxygen results in a very steep redox gradient. Predominantly, muddy sediments face chemical
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conditions changing across a few millimetres. While oxygen is used by organisms in the
surface layers, nitrate and sulphate act as electron donors in deeper layers prior to the
reduction zone. In the reduction zone compounds as sulphur, nitrogen, iron and manganese
are present. Due to these manifold conditions sediments harbour the largest variety of
metabolic types of microorganisms (Sommer 2005). Depending on the granular structure
108 -1011 bacterial cells per millilitre can be observed in marine sediments. Thereby bacterial
biomass is increasing with decreasing grain size. Generally, sandy sediments are less
colonised since they offer less volume-specific surface area and less nutrients then muddy
sediments (Yamamoto and Lopez 1985).
Because of their diverse metabolic capabilities and high enzymatic activities microbial
communities play a crucial role in biogeochemical cycling (Pomeroy 1974). Principally,
heterotrophic, phototrophic and lithotrophic bacteria can be found in sediments. Depending
on the availability of electron donors and acceptors, various metabolic types exists. For
instance: aerobic heterotrophs, aerobic and anaerobic chemolithotrophs, reducers and
oxidisers of manganese, iron and sulphate, methanogens and methanothrophs, as well as
fermentative bacteria (Nealson 1997). The metabolic processes of these bacteria result in a
continuous release and resuspension of nutrients from the seafloor. Upwelling processes or
storm events transport the nutrients in the photic zone where they stimulate phytoplankton
and bacterial growth (Marcus and Boero 1998). These in turn stimulate the zooplankton and
in this manner the whole food chain. Because not all organisms are consumed by planktonic
grazers they eventually die and sink down on the seafloor. This process is known as benthicpelagic coupling (Marcus and Boero 1998). The impact of organic material input on benthic
bacterial communities was already subject in many studies (Franco et al 2007, Graf et al
1982). It was concluded that the input of organic matter leads to changes in the bacterial
community structure, bacterial biomass and productivity (Franco et al 2007, Graf et al 1982,
Meyerreil 1983).
Bacterial community composition
The bacterial community in marine sediments is dominated by gram-negative Proteobacteria.
Moreover, members of the phyla Bacteroidetes, Planctomycetes and Chloroflexi contribute to
the bacterial community of the marine benthos. The phylum of Proteobacteria includes
various metabolic types. Principally they are divided into five classes: Alpha-, Beta-,
Gamma -,
Delta-
and
Epsilonproteobacteria.
In
marine
sediments
Delta-
and
Gammaproteobacteria dominate the bacterial community. While Deltaproteobacteria
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constitute a physiological homogeneous group, comprising almost all sulphate reducing
species, Gammaproteobacteria contain various physiological groups. Vital members of the
chemoorganotrophic
Gammaproteobacteria
are
the
genera
Alteromonas
and
Pseudoalteromonas as well as the genera Oceanospirillum or Marinobacter which form a
separate clade. The phylum of Bacteroidetes contains the Cytophaga-Flavobacteria cluster as
well as the Bacteroides subgroup. Firstly described by Winogradsky (1929), members of the
Cytophaga-Flavobacteria cluster are characterised as unicellular, gliding, nonespore-forming
rods. This group comprises members featuring various physiological capabilities,
furthermore, they are adapted to a broad range of environmental conditions (Weller et al
2000). Generally, Bacteroidetes are strongly associated with the water column and marine
aggregates. But some studies described their abundance also for aerobic and anaerobic
sediments (Llobet-Brossa et al 1998, Ravenschlag et al 2001). Flavobacteria are believed to
play a pivotal role in the degradation of organic matter since they own hydrolytic capabilities
(Abell and Bowman 2005, Cottrell 2000). The phyla Planctomycetes and Chloroflexi occur in
all natural environments and were detected also in North Sea sediments (Kittelmann and
Friedrich 2008, Webster et al 2007). The phylum Planctomycetes represents in several ways
an exceptional group. Members have cell walls that are not composed of peptidoglycan.
Additionally, some species feature an intracellular compartment that contains DNA. Green
non-sulfur bacteria or Chloroflexi comprise various phenotypes. Including species gliding
filamentous and isolates that contain some sort of bacteriochlorophyll frequently arranged in
chlorosomes (Rappe and Giovannoni 2003). The structure of benthic bacterial communities
however is substantially determined by environmental conditions.
Bacterial communities in estuaries: Effects of physicochemical and biogeochemical
variations and pollution
Studies conducted on benthic bacterial communities aim to investigate their community
composition in variable or permanently cold marine habitats (Dale 1974, Llobet-Brossa et al
1998, Ravenschlag et al 1999), their ecological role in various nutrient cycles, examine the
influence of organic material inputs (Duyl et al 1992, Meyer-Reil and Koster 2000) or
contaminant input (Paisse et al 2008) on the bacterial community. Spatial investigations
revealed that predominantly salinity, pH, and nutrients such as ammonium and phosphate
shape the bacterial community assembly in estuaries (Sun et al 2011). Additionally, Bowen
and co-workers (2009) suggested that habitat-specific forces determine the sediment bacterial
communities in salt marsh environments. However, to date most studies focus on pelagic
bacterial communities in estuaries (Bouvier and del Giorgio 2002, Crump et al 1999,
5
Fortunato and Crump 2011, Fortunato et al 2012, Herlemann et al 2011, Selje and Simon
2003). Generally, pelagic bacterial communities appear to be rather influenced by spatial
factors such as depths or salinity than by temporal factors. Herlemann and co-worker (2011)
as well as Selje and co-workers (Selje and Simon 2003) observed distinct bacterial
community cluster for marine, freshwater and brackish water environments. Spatiotemporal
investigations of bacterial communities in estuaries, however, are rare. To our knowledge
only Fortunato and co-workers (2012) considered the impact of spatial and temporal
variations on pelagic bacterial communities in estuaries, while these studies are lacking for
benthic bacterial communities.
Anthropogenic perturbation represents a major concern especially in coastal areas as already
mentioned above. Hence, several studies have addressed the impact of perturbation on
bacterial communities (Dean-Ross and Mills 1989, Gillan et al 2005, Roling et al 2001, Wang
et al 2011). It was highlighted that bacterial communities react to physical disturbance, as
sieving, with changes in community structure and reduced biomass (Findlay et al 1990).
Observations of the impact of heavy metal or oil contamination on bacterial communities
revealed that the contamination affects the structure as well as the function of bacterial
communities (dos Santos et al 2011, Gremion et al 2004, Suarez-Suarez et al 2011). Even the
impact of ocean dumping on bacterial communities was studied, but predominantly in
mesocosm experiments so far (Kan et al 2011, Nayar et al 2004, Toes et al 2008). Respective
field studies are lacking until today.
To our knowledge, investigations of benthic bacterial communities of sublittoral sediments in
the German Bight are scarce. More detailed information about benthic bacterial communities
inhabiting sublittoral sediments will help us to better understand ecological processes and
anthropogenic interferences in coastal environments.
Methodological approaches
Nowadays, the range of molecular approaches to describe microbial communities is extremely
broad. Community structure and composition is mainly estimated by fingerprinting and
sequencing approaches. Most applications, for both community analyses and phylogenetic
studies, base on the highly conserved small-subunit (SSU) ribosomal genes. Apart from its
highly conserved DNA sequence SSU ribosomal genes feature highly variables regions and
finally the possibility to align the sequence information to a vast number of data bases in
order to analyse phylogenetic relationships. Functional diversity of bacterial communities is
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addressed in RNA approaches and as newly invented microarray approaches targeting
functional genes (He et al 2007).
Denaturing Gradient Gel Electrophoresis (DGGE) represents probably the most common
fingerprinting method in microbial ecology. This method does not only provide insight into
the community structure and dynamics, moreover the amplified and separated 16S rDNA
fragments may be used in sequencing approaches to identify the represented phylotypes.
Further applications are Amplified Ribosomal DNA Restriction Analysis (ARDA), Terminal
Restriction Fragment Length Analysis (T-RFLP), and Automated Ribosomal Intergenic
Spacer Analysis (ARISA). In contrast to DGGE the ARISA fingerprinting bases on the length
polymorphism of the intergenic spacer region located between 16S and 23S rDNA. Basically,
the length of this region is species-specific and ARISA fingerprinting resolves therefore
phylotypes more deeply compared to DGGE (Okubo and Sugiyama 2009). The method
ARISA was applied in the presented thesis to investigate the structure of benthic bacterial
communities.
In recent years sequencing methods faced a fast development of alternatives to the
conservative sanger sequencing approach. 454 Life Sciences invented a new generation of
sequencing, named often “high-through put sequencing” or “next generation sequencing”,
capable of hundreds of thousands reads in parallel. The technique bases on an emulsion PCR.
Simultaneously millions of PCR reactions, separated by oil droplets, are taking place. The
advancement of sequencing methods offered new capabilities to explore microbial community
composition (Schuster 2008).
Microarrays finally, enhanced the analysis of functional structures of microbial communities.
The principle of microarray technology bases on small single stranded oligonucleotide probes
(specific DNA sequences), which are immobilised on a solid phase (generally glass or
silicon). For analysis of environmental samples fluorescently labelled single stranded DNA
from a certain sample is applied on the microarray. Strong hydrogen bonds between
complementary nucleotide base pairs hybridise the target DNA to the specific probe on the
microarray. Non-specific bindings of probes are removed by washing steps and only strongly
hybridised double strains remain. The signal generated by the labelled target DNA can be
quantified. Generally, the signal intensity depends on the amount of target DNA bound to the
probe. The functional gene array GeoChip, firstly introduced in 2007 (He at al 2007)
encompasses probes from genes involved in key microbial mediated biogeochemical
processes (e.g. carbon, nitrogen and sulphur cycling as well as organic contaminant
7
degradation and metal resistance and reduction. Initially invented for soil communities
(He et al 2007), the GeoChip was recently implemented in marine (Wang et al 2009) and
contaminated habitats (Liang et al 2009, Lu et al 2012). The latest version of this microarray,
GeoChip 4.2, contains DNA probes targeting functional groups of carbon, nitrogen, sulphur
and phosphorus cycling, metal and antibiotic resistance, energy process, organic contaminant
degradation, stress and virulence. In the framework of this thesis we utilised the GeoChip 4.2
to analyses the functional structure of representative bacterial communities from a dumping
site.
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__________________________________________________________________________________
RESEARCH AIMS
The aim of this thesis was to gather more detailed information about benthic bacterial
communities in the German Bight. Bacterial communities of sublittoral shelf sediments in the
German Bight remain widely uncharacterised. Many questions concerning their distribution in
particular, referring different environmental conditions, both spatial and temporal, remain
unclear. We conducted monthly cruises along transects in the German Bight to observe
bacterial community variations on temporal and spatial gradients. Another major part of this
thesis focuses on the impact of dumping activities on benthic bacterial communities.
Spatiotemporal gradients influencing benthic bacterial communities in near and
offshore regions in the German Bight
Spatial and temporal variations of benthic bacterial communities along three transects in the
German Bight were characterised. Sediment samples were collected monthly over one year.
Each transect offered unique geochemical and physicological conditions. Bacterial
communities inhabiting the sediments along the transects were followed over a seasonal
cycle. Simultaneously, physico-geochemical parameters such as grain size distribution,
carbon content, temperature, salinity and chlorophyll a were recorded. Fingerprints of the
bacterial community structure were obtained via Automated Ribosomal Intergenic Spacer
Analyses (ARISA). The conjunction with environmental variables was realised in
multivariate multiple regression analyses.
Characterisation of benthic bacterial communities at a dumping site: investigating
bacterial community structure and function
Anthropogenic perturbation represents an issue of great concern also in regard to bacterial
community response. We investigated the impact of an active dumping site on bacterial
communities in the German Bight. For this approach we followed an existing sampling
scheme for monitoring of geochemistry and macrozoobenthos. In three sampling campaigns
sediment samples were obtained at 125 sampling positions. Bacterial community profiles
were obtained via ARISA. Fingerprinting profiles were statistically analysed also related to
environmental parameters. To yield information about the community composition
representative samples were subjected to SSU ribosomal tag sequencing.
Our investigations of bacterial communities at a dumping site in the German Bight were
completed by subjecting representative samples to functional gene arrays. We utilised the
GeoChip 4.2, a gene array targeting functional genes of carbon, nitrogen, sulphur and
9
phosphorus cycling, metal and antibiotic resistance, energy process, organic contaminant
degradation, soil benefit, soil borne pathogens, stress and virulence. The functional structure
of the microbial communities was furthermore related to environmental parameters (e. g.
pollutants, grain size).
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__________________________________________________________________________________
OUTLINE
This cumulative thesis consists of three chapters; each representing a stand-alone publishable
manuscript
Chapter I (in preparation for submission to the ISME Journal)
Störmer, R., Wichels, A., Gerdts, G.
Spatiotemporal variations of benthic bacterial communities in the German Bight
The planning, analyses and manuscript writing were carried out by Rebecca Störmer under
the guidance of Antje Wichels and Gunnar Gerdts. Sampling was conducted by Rebecca
Störmer, Kristine Carstens, Sylvia Peters and Julia Haafke. CHN analyses were performed by
Rebecca Störmer and Julia Haafke. Christian Hass assisted with the grain size analysis of the
sediments. Salinity, temperature and chlorophyll a data were kindly provided by Karen H.
Wiltshire.
Chapter II (submitted to the Marine Pollution Bulletin)
Impact of ocean dumping on bacterial communities I: Fine-scale investigations at a
dumping site
Störmer, R., Wichels, A., Gerdts, G.
the guidance of Antje Wichels and Gunnar Gerdts. Sampling was performed by Rebecca
Störmer and the contextual data were kindly provided by the Hamburg Port Authority. Jörg
Peplies assisted with the sequencing analyses.
Chapter III (submitted to the Marine Pollution Bulletin)
Impact of ocean dumping on bacterial communities II: GeoChip-based analysis of
bacterial communities at a dumping site
Störmer, R., Wichels, A., Gerdts G.
the guidance of Antje Wichels and Gunnar Gerdts. Sampling was performed by Rebecca
Störmer and contextual data were kindly provided by the Hamburg Port Authority. Samples
11
for functional gene analyses were conducted by Glomics, Inc.. Zhili He and Joy van Nostrand
assisted with the interpretation of the data.
.
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CHAPTER I
__________________________________________________________________________________
CHAPTER I
Biogeography of benthic bacterial communities in the German Bight
Rebecca Störmera, Antje Wichelsa, and Gunnar Gerdtsa
a
Microbial Ecology Group Alfred Wegener Institute for Polar and Marine Research
Kurpromenade 201, 27498 Helgoland, Germany
rebecca.stoermer@awi.de, antje.wichels@awi.de, gunnar.gerdts@awi.de
13
Abstract
Studies investigating the biogeography of benthic bacterial communities on spatiotemporal
scales in different marine habitats are rare. This study presents spatiotemporal variations of
benthic bacterial communities in near and offshore regions of the German Bight (North Sea).
Bacterial community structure and diversity were estimated from Automated Ribosomal
Intergenic Spacer Analysis (ARISA). Relationships between bacterial community structure
and environmental factors were disentangled in multivariate multiple regression models. We
observed temporal and spatial variations of bacterial communities in nearshore regions.
Bacterial communities in offshore regions however, were highly dispersed and only the
diversity showed seasonal variations. Temporal factors appeared to be most important in
shaping the benthic bacterial communities in nearshore regions. Spatial variations of the
bacterial communities were strongly linked to respective strong environmental gradients
(sediment composition, salinity) occurring in the individual nearshore regions.
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CHAPTER I
__________________________________________________________________________________
Introduction
Abundance and distribution of species and factors influencing them are crucial to understand
ecosystem functioning and to predict environmental changes. It is widely agreed that bacterial
biogeography is influenced by a multitude of biotic and abiotic factors (Fuhrman et al 2006,
Graham 2004, Lozupone and Knight 2007, Yannarell et al 2003a). Fuhrman and co-workers
(2006) stated that bacterial community composition is predictable from ocean conditions.
They highlighted that bacterial community assembly in the ocean is depended on various
abiotic and biotic factors but that temporal changes appear to be the most important ones. In
contrast, considering various ecosystems (soil, marine, freshwater) Lozupone and Knight
(2007) stated that most importantly salinity variations determine the bacterial community
composition. The comparison of these two studies demonstrates the necessity of individual
studies in individual ecosystems. Gaining more information about factors influencing
bacterial community structure in individual ecosystems will help to model and predict
bacterial community responses to certain environmental short time events (e.g. nutrient input)
and to predict longterm consequences for instance in the context of climate change or
environmental pollution.
Plenty of studies aim to determine spatial and temporal factors influencing bacterial
community structure (Acinas et al 1997, Allan and Froneman 2008, Boer et al 2009,
Ghiglione et al 2005). Most studies focus on specific environments such as estuaries
(Fortunato and Crump 2011), coastal areas (Alonso-Saez et al 2007) or the open ocean
(Fuhrman et al 2006). To our knowledge investigations of different environments, for
instance offshore and nearshore regions on spatiotemporal scales remain scarce.
Seasonal variability has been explored extensively for marine bacterial communities (AlonsoSaez et al 2007, Boer et al 2009, Gerdts et al 2004). Environmental factors determined by the
season such as temperature (Gonzalez-Acosta et al 2006), nutrient input (Jacquet et al 2002)
or primary production (Franco et al 2007, Meyerreil 1983) affect bacterial community
structure, biomass and productivity.
Spatial variability was most likely investigated along estuaries. Estuarine environments are
characterised by strong environmental gradients resulting from the mixing of fresh and marine
water masses at river mouths. Many of these gradients, including salinity, nutrient
concentrations and especially on the seafloor, sediment transports, may influence bacterial
communities. The high variability of this ecosystem makes it a perfect model system to study
15
spatial variations in community structure. Several studies described pelagic bacterial
communities in estuaries (Crump et al 2004, Fortunato and Crump 2011, Selje and Simon
2003). These studies demonstrated that bacterial community variations depend on both abiotic
and biotic gradients. However, most of them focus on the impact of salinity gradients on the
bacterial communities. Herlemann (2011) and co-workers as well as Selje and Simon (2003)
demonstrated the formation of distinct bacterial communities along salinity gradients. Both
studies showed typical marine, freshwater and brackish water groups. Generally, regarding
pelagic bacterial communities, the influence of spatial factors seems to overwhelm temporal
impacts on the bacterial communities. Spatiotemporal variations of benthic bacterial
communities in coastal areas remain widely uncharacterised. Especially in coastal areas
benthic bacterial communities’ contribute to a pivotal extent in remineralisation processes of
organic matter (Atlas and Bartha 1987). The input of organic matter from the euphotic zone to
the seafloor and the response of benthic communities is described by the term benthic-pelagic
coupling. Benthic-pelagic coupling is important in coastal areas as well as open waters (Graf
1989, Marcus and Boero 1998). In any case the input of organic material, resulting from
dying organisms in the water column, determines substantially the benthic community: To
date detailed information of these processes regarding benthic bacterial communities in
coastal areas are scarce.
The German Bight (North Sea) encloses the estuaries of Ems, Jade, Weser, Elbe, and Eider
Rivers. Studies of the past 50 years carried out in the German Bight were addressing mainly
eutrophication (Hickel et al 1993, Rachor 1990), pollution (Bester et al 1998, Gee et al 1992,
Schwarzbauer et al 2000, Vauk and Schrey 1987) and storm surges (Woth et al 2006). Long
term studies suggest a climate change in North Sea waters (Wiltshire et al 2010). Over the
past 50 years distinct changes in the hydrography and biota around Helgoland, an island
situated in the German Bight, going along with increasing temperature and salinity were
recorded. Summarising these efforts it becomes obvious, that in particular the German Bight
represents a highly variable ecosystem.
Pelagic bacterial communities in the German Bight were explicitly described in the last
decades (Eilers et al 2000, Eilers et al 2001, Gerdts et al 2004, Oberbeckmann et al 2011,
Sapp et al 2007, Teeling et al 2012). Benthic bacterial communities of the shelf sediments in
the German Bight remain poorly characterised. Some effort has been made on characterising
bacterial communities in the East Frisian Wadden Seas (Stevens et al 2005), subtidal
sediments in the Sylt-Romo basin (Boer et al 2009) intertidal sand flats at Sylt
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CHAPTER I
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(Musat et al 2006) and nearshore intertidal mud and sand flats of Dangast (LlobetBrossa et al 1998). The community composition was concluded to be stable over time but
differed for the individual investigated environments. Exceptional Boer and co-workers
(2009) described a large depth and time related variation within bacterial communities in
subtidal sediments in the Sylt-Romo basin. To our knowledge not a single study was
conducted investigating benthic bacterial communities of the sublittoral shelf sediments in the
German Bight. The lack of spatiotemporal investigations on benthic bacterial communities
inhabiting different sublittoral shelf sediments in combination with existing knowledge about
responses of pelagic bacterial communities in the corresponding pelagic habitats builds the
basis for our investigation.
We hypothesise that the bacterial community structure is determined by individual
environmental gradients in individual environments. Therefore spatiotemporal patterns of
benthic bacterial communities along three, according to their biogeochemical and
physicochemical parameters, unique transects were characterised. Geo- and physicochemical
parameters, in particular grain size distributions, organic carbon content, temperature, salinity
and chlorophyll a as a measure for phytoplankton abundances were recorded. Bacterial
community structure was obtained via automated ribosomal intergenic spacer analysis
(ARISA). The relationship between environmental factors and bacterial communities was
investigated using multivariate multiple regression models.
17
Material and Methods
Location of transects and sampling
Fig. 1 Overview of the three investigated transects in the German Bight. I: P8 transect, II: Elbe transect, III:
Eider transect.
Table 1 Sediment classification after Folk (1980).
Station
Sediment type
Station
Sediment type
Station
Sediment type
P8 II
P8 III
P8 IV
P8 V
P8 VI
Fine sand
Fine sand
Fine sand
Very fine sand
Very fine sand
Elbe II
E3
Elbe III
Elbe IV
Elbe V
Elbe VI
Coarse silt
(Very) Coarse silt
(Very) Coarse silt
Very fine sand
Fine sand
Fine/Medium sand
Eider I
Eider II
Eider III
Eider IV
Eider V
Eider VI
Fine sand
Fine sand
Fine/Medium sand
Fine sand
Fine/Medium sand
Fine sand
Starting from the German island Helgoland, North Sea (54°10’ N, 7° 53’ E) three transects
(Fig. 1, I: P8, II: Elbe and III: Eider) comprising in total seventeen stations were sampled.
Water depths were ranging from 53 – 8 metres. Sediments were classified according to Folk
(Folk 1980, Table 1). The sampling was performed monthly from September 2010 to July
2011. All sediment samples were taken with a van Veen grab (0.2 m³). Onboard, the sediment
was poured into a clean box and homogenised. To ensure coherent analyses, the samples for
18
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analyses of the microbial communities as well as the samples for CHN and grain size analyses
were taken from this sediment homogenate. Temperature and salinity data were obtained from
bottom water. For microbial community analysis, three subsamples were stored immediately
after collection at -20°C in 50 ml falcon tubes.
DNA-Extraction and Quantification
For DNA-Extraction the PowerSoil Kit (MoBio Laboratories, Carlsbad, CA, USA) was used
following the manufactures protocol. Per station three subsamples of 0.25 g sediment each
were subjected to the procedure. The extracted DNA was eluted in 50 µl elution buffer.
Genomic DNA concentrations were measured by photometry using the Infinite M200 (Tecan
Austria GmbH, Gröding, Austria). The DNA was measured in duplicate. DNA was also
controlled regarding the presence of proteins at 280nm (ratio > 1.8).
Automated Ribosomal Intergenic Spacer Analysis (ARISA)
Automated ribosomal intergenic spacer analysis was performed as previously described
(Störmer et al 2012).
OTU Definition for ARISA
ARISA fingerprint data were processed as previously shown (Störmer et al 2012).
Fingerprinting profiles of each sample were converted to “consensus fingerprinting profile”
(presence/absence) since environmental data were recorded only once per sample from each
site. Calculating the “consensus fingerprinting profile”, only fragments present in at least two
of the subsamples were regarded as present.
Environmental data analysis
CHN analyses
For CHN analyses samples were dried in a freeze dryer. Afterwards the sediments were
homogenised with a mortar. 30 mg sediment was filled in silver cups. In order to remove
organic carbon compounds HCL was added. The filled silver cups were then dried again at
100°C over night. Before application the Vario MICRO cube (elementar, Hanau, Germany)
the silver cups were encapsulated with tin cups in order to achieve optimal combustion
conditions (Hedges and Stern 1984).
19
Grain size distribution
Sediments were treated with acetic acid (33 %) and hydrogen peroxide (10 %) in order to
remove organic substances from the samples. The sediment was stored in water until analysis.
Grain size analysis was performed via CILAS 1180 laser particle analyser as previously
described (Dolch and Hass 2008).
Salinity, Chlorophyll a, Temperature
These data were obtained as part of the Helgoland Roads LTER series (Wiltshire et al 2008).
The data set was kindly provided by Karen H. Wiltshire.
The Helgoland Roads time series is accessible via the open database Pangaea
(http://www.pangaea.de).
Statistics
Univariate analysis
Differences regarding alpha diversity estimated from ARISA OTU numbers respecting spatial
(site) and temporal (month) differences were tested using one-way analysis of variance
(ANOVA, Statistica Version 7.1, StatSoft GmbH, Hamburg, Germany) for individual
transects. A significance level of p < 0.05 was applied. Pairwise comparisons of the samples
were tested in post hoc Tukey HSD tests (p < 0.05).
Pairwise correlations (Statistica Version 7.1, StatSoft GmbH, Hamburg, Germany) of all
environmental variables were performed with Spearman´s rank correlation (p < 0.05).
Multivariate analyses
The PERMANOVA subroutine PRIMER v6 (Clarke and Gorley 2006) with fixed factors was
employed to investigate “consensus fingerprinting profiles” of individual stations and months
for significant differences regarding their community structure. A significance level of
p < 0.01 and unrestricted permutation of raw data was applied.
Principal coordinates analysis (PCO) was performed to investigate inter-point dissimilarities
between the “consensus fingerprinting profiles” of samples for each transect individually. The
Jaccard index was applied to calculate the resemblance matrix for the “consensus
fingerprinting profiles”. The relationship between “consensus fingerprinting profiles” and
environmental variables was investigated by distance-based multivariate multiple regression
(DISTLM). Environmental variables, precisely: TOC, chlorophyll a, temperature, salinity and
grain size fractions were log transformed prior to the analysis. Jaccard Index was applied to
calculate the resemblance matrix for “consensus fingerprinting profiles”. The DISTLM model
was built using stepwise selection, adjusted R² and applying 4999 permutations at a
20
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significance level of p < 0.01. Results were visualised by using distance-based redundancy
analysis (dbRDA).
Results
Physicochemical and geochemical properties along the transects
Mean values and respective standard deviation for temperature, chlorophyll a, fine sand and
salinity are depicted in the Figures 2-4 for the individual transects. All data were obtained
from bottom water samples. Annual temperature and chlorophyll a followed a similar trend
along all three transects. Highest temperature occurred in June and October (~ 15°C, Fig. 2A4A). Highest chlorophyll a concentrations were observed in May along Eider and Elbe
transect (Elbe: ~ 20µg/l, Fig. 3B and Eider: ~ 10µg/l Fig. 4B). Spatial variations regarding
fine sand and salinity are shown in the figures (2C and D – 4C and D). The Elbe transect
displayed highest variations regarding fine sand distributions (Figure 3D). The sediment at the
sampling sites I-III had almost no fine sand fractions while they increased up to 60 % at
sampling site V (Fig. 3D).
Fig.2 P8 transect: Means of annual temperature and chlorophyll a variations (A,B) and spatial fine sand and
salinity variations (C,D).
21
Fig.3 Elbe transect: Means of annual temperature and chlorophyll a variations (A,B) and spatial fine sand and
Variations observed along the other transects were considerably lower ranging in general
between 20 – 40 % fine sand for individual sampling sites (Fig. 2D-4D). The steepest salinity
gradient was detected along the Eider transect (Fig. 4C). Salinity decreased from sampling
site I to VI from ~ 33 to ~ 25. In contrast salinity was rather stable along both Elbe and P8
transect.
Bacterial community structure
The bacterial community structure based on “consensus fingerprinting profiles” was subjected
to PERMANOVA and principal coordinates analysis (PCO) for each transect individually.
PERMANOVA was performed to investigate bacterial community structure for significant
differences respecting spatial (site) and temporal (month) factors. Furthermore alpha diversity
estimated from ARISA OTU numbers was investigated for significant spatial and temporal
differences. Certain months or sampling sites for individual transects are missing due to failed
sampling cruises.
22
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Fig.4 Eider transect: Means of annual temperature and chlorophyll a variations (A,B) and spatial fine sand and
Figure 5B and 5C depict the PCO plots of bacterial communities along the P8 transect
labelled according to respective sampling sites (Fig. 5B) and respective sampling months
(Fig 5C). The first two axes of the PCO for bacterial community structure along the P8
transect captured 30.8 % of the total variation. Neither distinct spatial nor temporal patterns
within the bacterial communities were observed (Fig. 5B and 5C). Consistent with the results
from the PCO, pairwise comparisons indicated no significantly different bacterial
communities respecting the sampling site. However, respecting the temporal factor (month)
significant differences comparing bacterial community structures from January and May were
shown (PERMANOVA, p < 0.01).
23
Fig. 5 Bacterial community analyses for the P8 transect. Location of the P8 transect (A), Plot of principal
coordinates analyses (PCO) of bacterial community fingerprints based on the Jaccard index referring to sampling
site (B) and month (C). Plots of distance-based redundancy analysis (dbRDA) of bacterial community
fingerprints and environmental variables based on the Jaccard index referring to sampling site (D) and month
(E). Significant environmental variables depicted in red (p < 0.01). Bar charts of means of ARISA OTU numbers
and respective standard deviation referring to sampling site (F) and month (G).
24
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Fig. 6 Bacterial community analyses for the Elbe transect. Location of the Elbe transect (A), Plot of principal
25
Fig. 7 Bacterial community analyses for the Eider transect. Location of the Elbe transect (A), Plot of principal
26
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PCO plots of the bacterial communities along the Elbe transect are shown in Figure 6B and
6C. Regarding spatial variation bacterial communities from sampling sites near the estuary
cluster together and are clearly separated from bacterial communities of the marine sampling
sites (Fig. 6B). Respecting the sampling month bacterial communities obtained from early
summer to autumn appear more similar when compared to the bacterial communities obtained
from winter and spring (Fig. 6C). Pairwise comparisons of bacterial communities via
PERMANOVA approach confirmed significant differences for spatial and temporal factors
(p < 0.01).
Bacterial communities of the Eider transect are displayed in Fig. 7B and 7C. The first two
axes of the PCO captured 31.7 % of the total variation. Generally, samples obtained near the
estuary separated from those of marine sampling sites (Fig. 7B). Furthermore distinct
community patterns were observed for the early summer to autumn and winter to spring
period (Fig. 7C). Consistent with the PCO pairwise comparisons of bacterial communities
revealed principally significant differences for marine and near estuary communities as well
as for early summer to autumn communities and winter to spring communities
(PERMANOVA, p < 0.01).
The alpha diversity is depicted as bar charts of mean values with respective standard deviation
of ARISA OTU numbers (Fig. 5-7F and 5-7G). Significant spatial (site) and temporal (month)
differences were tested with ANOVA and post hoc Tukey tests. We observed no significant
spatial differences for the three transects (Fig. 5-7F). Generally, lowest alpha diversity was
observed along the P8 transect. Means of ARISA OTU numbers ranged about 20 at the
individual sites (Fig. 5F). Significantly higher ARISA OTU numbers (~ 50 ARISA OTUs,
p < 0.05) were detected in May and October (Fig. 5G). As observed for the P8 transect
significant higher ARISA OTU numbers were observed for May along the Elbe and Eider
transects. Moreover the Elbe transect showed significantly higher ARISA OTU numbers in
June (p < 0.05).
Relation of bacterial community fingerprints to environmental data
We applied multiple regression analysis (DISTLM) to bacterial community data and
environmental variables for the individual transects. Prior to the analysis spearman’s rank
correlation revealed that generally silt and clay fractions were significantly strong correlated
with each other (rs > 0.87, Supplement 1). The same was observed for nitrogen, hydrogen and
TOC content (rs > 0.68, Supplement 1). For the Elbe and Eider transect significant negative
27
correlations for medium and fine sand fractions with silt and clay fractions were observed
(rs > 0.69, Supplement 1). Significant correlations were also observed for salinity, nitrogen,
hydrogen and TOC with silt and clay fraction for both Elbe and Eider transects (rs > 0.34,
Supplement 1).
The results obtained by DISTLM are depicted in distance-based redundancy analyses
(dbRDA, Fig. 5D and 5E). The first two axes of the dbRDA of the P8 transect explain 23.6 %
of the total and 40.3 % of fitted variation. This indicates that the plot captures most of the
salient patterns in the fitted model. Marginal and sequential tests indicated solely chlorophyll
a concentrations to have a significant effect on the bacterial community structure (Table 2).
However chlorophyll a contributes solely with 0.08 % to the model. The dbRDA shows,
consistent with the results obtained from PCO and PERMANOVA no clear patterns of
bacterial community structures. The results for the Elbe transect are displayed in Fig. 6D and
6E. Here, 23.2 % of the total and 49.8 % of the fitted variation are covered. Medium and fine
sand as well as silt fractions and clay, temperature, salinity and chlorophyll a had a significant
individual effect on bacterial community structure as revealed by marginal test in the
DISTLM model. However regarding the sequential tests solely temperature, fine sand and
chlorophyll a had significant effects (Table 2).
The factors contribute with 22.8 % to the model (Table 2). Observing the dbRDA plots
temperature is rather associated with the first axis of the dbRDA while fine sand is correlating
with the second axis (Fig. 6D and 6E). Regarding the spatial aspect (site, Fig. 6D); the
environmental variable fine sand forms a strong gradient separating bacterial community
structures from the stations Elbe V and Elbe VI from the other stations. Temperature on the
other hand separates bacterial communities from May, June and October from the other
months (Fig. 6E).
Bacterial community structure along the Eider transect however is significantly influenced by
individual effects of temperature, salinity and chlorophyll a (Fig. 7D and 7E, Table 2). In the
sequential tests significant effects for temperature and salinity were confirmed (Table 2). Both
variables contribute with 22.1 % to the model. Again, temperature is rather correlated with the
first axis forming a strong gradient which separates bacterial communities from April, May,
June and October from the other months (Fig. 7E). The effect of salinity is rather spatial since
bacterial communities from the sites Eider I – III correlate with increasing salinity (Fig. 7D).
28
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Table 2 DISTLM results for bacterial community data and environmental factors.
P8
Variable
Pseudo-F
Coarse gravel
Medium gravel
Fine gravel
Coarse sand
Medium sand
Fine sand
Coarse silt
Medium silt
Fine silt
Clay
Temperature
Salinity
Nitrogen
TOC
Hydrogen
Chlorophyll a
0
0
0
0,99048
0,90207
0,70197
0,73036
0,68893
0,72466
0,69247
16.363
0,8463
19.092
0,58459
13.384
20.573
P
1
1
1
0,4648
0,5728
0,8086
0,7747
0,817
0,7769
0,8073
0,0493
0,6443
0,0133
0,9132
0,1625
0,0093
Proportion of
variance
Sequential test
0,000
0,000
0,000
0,041
0,038
0,030
0,031
0,029
0,031
0,029
0,066
0,035
0,077
0,025
0,055
0,082
Chlorophyll a
Nitrogen
Temperature
Medium sand
Fine sand
Salinity
Coarse silt
Fine sand
Clay
Hydrogen
TOC
Coarse sand
Medium sand
Pseudo-F
P
Proportion of
variance
20.573
15.993
11.142
12.806
10.496
0,90075
0,8506
12.235
1.049
0,86502
13.366
11.289
0,75638
0,0092
0,0617
0,3351
0,1882
0,3974
0,5591
0,6175
0,2462
0,3904
0,5824
0,2017
0,3468
0,6767
0,082
0,062
0,043
0,049
0,040
0,034
0,033
0,047
0,040
0,033
0,050
0,042
0,029
Elbe
Variable
Pseudo-F
Coarse gravel
Medium gravel
Fine gravel
Coarse sand
Medium sand
Fine sand
Coarse silt
Medium silt
Fine silt
Clay
Temperature
Salinity
Nitrogen
TOC
Hydrogen
Chlorophyll a
0
0
0
15.685
2.362
26.317
26.109
25.044
23.395
22.599
47.382
24.043
16.197
17.895
19.452
38.587
P
1
1
1
0,0425
0,0021
0,0007
0,0012
0,001
0,0024
0,0035
0,0001
0,0007
0,0468
0,0219
0,0106
0,0001
Proportion of
variance
Sequential test
0,000
0,000
0,000
0,041
0,060
0,066
0,066
0,063
0,060
0,058
0,114
0,061
0,042
0,046
0,050
0,094
Temperature
Fine sand
Chlorophyll a
Salinity
Hydrogen
Coarse silt
Medium sand
Coarse sand
Fine silt
Medium silt
Clay
Nitrogen
TOC
Pseudo-F
47.382
30.272
20.515
16.793
13.296
11.434
12.879
10.608
0,92303
12.812
10.797
0,77095
0,67199
P
0,0001
0,0001
0,0016
0,0132
0,1106
0,2703
0,1348
0,3847
0,5777
0,1628
0,3552
0,7846
0,8882
Proportion of
variance
0,114
0,069
0,045
0,036
0,029
0,024
0,027
0,022
0,020
0,027
0,023
0,016
0,014
Eider
Variable
Pseudo-F
Coarse gravel
Medium gravel
Fine gravel
Coarse sand
Medium sand
Fine sand
Coarse silt
Medium silt
Fine silt
Clay
Temperature
Salinity
Nitrogen
TOC
Hydrogen
Chlorophyll a
0
0
0
12.317
14.631
17.225
12.322
11.263
10.064
0,91645
48.452
24.958
0,65788
12.657
0,82147
4.022
P
1
1
1
0,1943
0,0918
0,0377
0,1967
0,2823
0,4245
0,5278
0,0001
0,0024
0,889
0,181
0,6721
0,0001
Proportion of
variance
Variable
0,000
0,000
0,000
0,035
0,041
0,048
0,035
0,032
0,029
0,026
0,125
0,068
0,019
0,036
0,024
0,106
Temperature
Salinity
Coarse sand
Medium sand
Fine sand
TOC
Nitrogen
Hydrogen
Clay
Coarse silt
Medium silt
Fine silt
Chlorophyll a
Pseudo-F
48.452
40.626
15.623
12.712
11.071
0,89848
10.825
0,93452
0,87536
15.997
12.701
0,83047
0,65908
P
0,0001
0,0001
0,0409
0,1559
0,3112
0,6015
0,3474
0,538
0,6317
0,0416
0,1845
0,687
0,8647
Proportion of
variance
0,125
0,096
0,036
0,029
0,025
0,021
0,025
0,022
0,020
0,036
0,028
0,019
0,015
29
Discussion
Temporal and spatial variations within bacterial communities are of great interest not only for
microbial ecology but also for modelling ecosystem functioning on a global scale. To date
most research focuses on either temporal (Fuhrman et al 2006, Kan et al 2006, Yannarell et al
2003a) or spatial variations within bacterial communities (Crump et al 2004, Herlemann et al
2011, Hewson et al 2007), nearly exclusively bacterioplankton communities were
investigated. Temporal as well as spatial variations appear to influence the community
structure tremendously (Fuhrman et al 2006, Herlemann et al 2011, Yannarell et al 2003b).
As main driving factors predominantly temperature and salinity are mentioned. Several
studies took both temporal and spatial scales into account (Fortunato et al 2012, Ghiglione et
al 2005, Hewson et al 2006). To our knowledge not a single one concentrated on benthic
bacterial communities. This study provides a unique perspective on how spatiotemporal
gradients influence benthic bacterial communities in a coastal area in the German Bight. We
investigated simultaneously benthic bacterial communities inhabiting near and offshore
environments over an annual cycle. The biogeography was assessed via ARISA fingerprinting
and main driving environmental factors were identified using multivariate multiple regression.
We hypothesised that bacterial community structure is determined by individual
environmental gradients in near and offshore regions.
Bacterial communities in near and offshore habitats
The three investigated transects in the German Bight differed greatly regarding influencing
biogeochemical and physicochemical parameters such as sediment composition, temperature,
salinity and chlorophyll a concentrations. We observed neither spatial nor temporal variation
within bacterial communities along the P8 transect, located > 60 kilometres offshore the
coastline. In contrast, bacterial communities along both Elbe and Eider transect varied
significantly regarding their community structure on both, temporal and spatial scales. Both
transects ended around 25 kilometres near the coastline. The P8 transect exhibited rather
stable conditions regarding recorded abiotic and biotic factors. Elbe and Eider transect in
contrast, end in the near of their respective estuaries and our data showed that they are
characterised by a high variability regarding physicochemical parameters such as salinity,
temperature or organic loading (Fig. 2). Especially in nearshore regions local winds might
lead to considerable shifts between coastal upwelling and downwelling conditions, while
offshore regions are less affected by local winds and physicochemical conditions remain
rather stable (Fig. 2). The pronounced spatial and temporal variations regarding
30
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physicochemical and biogeochemical parameters along the estuaries and the in contrast weak
variations along the P8 transect suggest the presence of two regimes differently impacted by
physical parameters. We assume that the distance to the coast and the implying different
impact of physical forces represents a major factor driving spatiotemporal variations within
the communities.
To our knowledge studies investigating spatial variations of benthic bacterial communities
comparing temperate nearshore and offshore habitats are scarce. Uthicke and co-workers
(2007) examined bacterial communities in coral reef sediments and observed, in line with our
investigation, significant differences between nearshore and offshore communities. The
separation of nearshore and offshore communities was also described for pelagic communities
(Fortunato and Crump 2011, Rink et al 2011).Only recently, Rink and co-workers (2011)
published their investigations of regional patterns of pelagic bacterial communities in the
German Bight. They assume that differences in the hydrographic and biogeochemical
conditions affect the assembly of the bacterial communities. We assume that benthic bacterial
communities display spatial variations but to a lesser extent compared to pelagic
communities.
In contrast to bacterial community structure bacterial diversity appears not to be affected by
spatial but explicitly by temporal factors. Principally, a significant higher alpha diversity was
observed for the period from May to October. This finding is in line with observations made
in Wadden Sea sediments in the Sylt-Romo basin (Boer et al 2009). Boer and co-workers
(2009) reported a higher diversity in August when compared to the other sampling months.
Especially in spring and autumn organic matter input can vary considerably due to changes in
the primary production in the North Sea (Duyl and Kop 1994). The primary production is
controlled by nutrients which resuspend from the seafloor into the photic zone. A high
nutrient availability stimulates the phytoplankton production and phytoplankton blooms
occur. These in turn stimulate the zooplankton and consequently the whole food chain.
Organisms which are not consumed in the water column die and sink to the seafloor
(approximately three metres per day in North Sea waters (Skogen et al 1995). Bacterial
communities respond with increasing productivity to organic matter input for instance after
phytoplankton blooms (Duyl and Kop 1994, Meyerreil 1983) and indications for increasing
bacterial diversity coupled to organic matter input and nematode diversity were stated by
Vanaverbeke and co-workers (2004). Bentho-pelagic coupling represents a crucial element for
benthic life. The input of pelagic particles sinking to the seafloor determines substantially
31
benthic communities. We assume that the increasing bacterial diversity is directly linked to
these processes.
Main influencing gradients along the three transects
Chlorophyll a, fine sand, salinity and temperature were identified as main factors influencing
the bacterial community structure along the individual transects.
Chlorophyll a concentrations had a significant effect on bacterial community structures along
P8 and Elbe transects. Chlorophyll a, an indirect measure for phytoplankton, was
considerably higher in May as compared to other sampling months (Fig. 2). As already
discussed in the previous section, phytoplankton blooms arise generally in spring and autumn
in the shallower regions in the North Sea (Joint and Pomroy 1993). They are characterised by
a distinct patchiness and are highly dynamic. Water movement, caused by currents and winds
transport the phytoplankton bloom from shallower coastal regions into deeper offshore
regions. Along with this movement productivity gradients from high productivity in nearshore
regions to low productivity in offshore regions establish (Joint and Pomroy 1993). This
productivity gradient of the phytoplankton was mirrored in our chlorophyll a data. We
observed highest chlorophyll a concentrations at coastal sampling sites along Elbe and Eider
transects compared to lower concentrations at offshore sampling sites along the P8 transect. In
May, however, relatively high chlorophyll a concentrations in the bottom water were
observed along all investigated transects representing probably a post-bloom signal. We
observed significant different bacterial community structures in May when compared to
bacterial communities in earlier months of the year. Again this might be an indication for
benthic-pelagic coupling. We hypothesise, even though the chlorophyll a concentrations were
measured in the bottom water, that the organic matter reached already the seafloor. Thus, the
benthic bacterial community responded with a simultaneous increase in bacterial diversity and
changes in the bacterial community structure to the input of organic material originating from
decaying phytoplankton blooms.
Spatial differentiation was assigned to fine sand and salinity variations for the individual
nearshore transects. While fine sand distributions affected bacterial communities along the
Elbe transect, bacterial communities clustered according to salinity variations along the Eider
transect. The Elbe transect passes a region which is characterised by (very) coarse silt at the
sites Elbe II, E3 and Elbe III while the sediment at the sites Elbe IV, Elbe V and Elbe VI was
composed of fine sand (Table 1, Fig. 2). The mud deposit in the south-east of Helgoland is
32
CHAPTER I
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well documented (Hebbeln et al 2003, Mühlenhardt-Siegel 1981, Puls et al 1997). The
continuous sedimentation in this area is caused by a small-scale eddy driven by the interaction
of the longshore coastal current, the discharge of Elbe and Weser Rivers and tidal dynamics
(Hebbeln et al 2003). Obviously, the bacterial communities in the sediments along the Elbe
transect are affected by the resulting grain size gradient. This assumption bases on the
significant individual effect of silt and clay fractions on the bacterial community variation as
revealed by our marginal tests (Table 2) and the significant impact of fine sand distributions
in the sequential tests coupled with the respective clustering of bacterial communities.
Sediment composition represents a major driving factor for benthic bacterial community
assembly (Dale 1974, DeFlaun and Mayer 1983). Only recently a study conducted at a
dumping site which is included in the Elbe transect (site E3) revealed a strong gradient of
grain size distributions which influenced significantly the bacterial community structure
(Störmer et al 2012). Principally, sandy sediments harbour different bacterial groups than
muddy ones (Llobet-Brossa et al 1998). We therefore conclude that bacterial community
structure is highly influenced by the steep grain size gradient along the Elbe transect.
The steepest salinity gradient was recorded along the Eider transect. Salinity ranged between
33-22 and defined therefore marine and estuarine conditions. We observed a distinct
clustering of bacterial communities according to this salinity gradient (Fig. 5). Salinity
gradients represent an important factor influencing bacterial communities in estuaries (Selje
and Simon 2003). Salinity contributes to density gradients in coastal areas which separate
water masses and their residential pelagic bacterial communities (Fortunato et al 2012).
Among others Herlemann and co-workers (2011) reported defined bacterial communities for
marine and fresh water as well as for the brackish water bodies. To our knowledge studies
addressing benthic bacterial community changes in estuaries according to salinity gradients
are little studied (Ikenaga et al 2010). However, Ikenaga and co-workers (2010) demonstrated
recently that benthic bacterial communities cluster along a salinity gradient in the Everglades.
Temporal variation among the bacterial communities was mainly explained by temperature
variations. For both nearshore transects (Elbe, Eider) seasonal changes in the bacterial
community structure were resolved. Principally, bacterial communities clustered according to
the early summer to autumn and winter to spring season. Regarding temperature these
communities might also be considered as warm and cold period communities. The
temperature effect implies in fact a multitude of other factors which change with temperature.
In coastal areas for instance nutrient input, river discharge, upwelling and productivity are
33
closely linked to temperature variations. Thus, benthic bacterial communities might not be
affected by temperature variations alone but by seasonal processes linked to temperature
variations.
Temporal variations were shown to explain most of the variance in our models (Table 2).
Therefore we assume that temporal variations are of great importance for benthic bacterial
community assembly. The study of Boer and co-workers confirms this hypothesis (Boer et al
2009). Studies investigating pelagic bacterial communities demonstrated contrary, that spatial
variations overwhelmed temporal factors (Fortunato et al 2012). Fortunato and co-workers
(2012) found that salinity and depth influenced the bacterioplankton predominantly. Probably
pelagic and benthic bacterial communities are affected by different factors in coastal regions.
It would be worth approaching this hypothesis by studying pelagic and benthic bacterial
communities simultaneously.
In summary our study allowed novel insights into bacterial community structure and diversity
along spatial and temporal gradients in the German Bight. We showed that bacterial
communities in offshore regions showed no clear temporal or spatial variations while their
counterparts in nearshore regions exhibited distinct temporal as well as spatial patterns.
Temporal variations were predominantly driven by temperature and of greater importance
than spatial gradients.
Acknowledgments
We would like to thank Prof. Dr. Karen Wiltshire for kindly providing salinity, temperature
and chlorophyll a data. The interpretation of our data would have been not possible without
this information. We thank Kristine Carstens, Sylvia Peters and Julia Haafke for sampling.
And finally Julia Haafke and Christian Hass for assisting with the CHN and grain size
analyses.
34
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CHAPTER II
Impact of ocean dumping on bacterial communities
I: Fine-scale investigations at a dumping site
a
Corresponding author: rebecca.stoermer@awi.de, phone: (0049)4725/819-3233, fax:
(0049)4725/819-3283
35
Abstract
The impact of ocean dumping on benthic bacterial communities is not included in regular
monitoring programs, yet. Hence, in 2009 and 2010, we initiated an extensive investigation of
the spatial structure of the bacterial community at a dumping site in the German Bight using
the fingerprinting method, Automated Ribosomal Intergenic Spacer Analysis. Using
redundancy analyses, we aimed to identify the main environmental factors shaping the
bacterial community. The phylogenetic composition was investigated via ribosomal tag
sequencing for representative samples. Our results reveal significantly different bacterial
communities when comparing dumping and a reference sites. Furthermore, ten months after
dumping the dumping centre displayed a low alpha diversity. Typical freshwater bacterial
phylotypes and Desulfuromonadaceae as well as Flavobacteriaceae were observed in
considerably higher numbers at the dumping centre. We assume, that most likely the sediment
granularity and to a lesser extent, pollutants, shape the bacterial community.
Keywords: ARISA/ dredged sediment / fingerprinting analysis / multivariate statistics/
pollution / 454 sequencing/
36
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Introduction
Estuaries represent economically significant areas, which are exposed to many types of
human interferences (Lotze 2010). Protective measures, such as dikes and the deepening of
commercial shipping lanes, alter natural hydrodynamics of rivers and estuaries (Freitag et al
2008). Naturally high siltation rates in these areas exacerbate the increase in the amount of
dredged material. Dumping sites for this dredged material and sewage sludge exist in many
coastal zones worldwide (OSPAR 2009, Stronkhorst et al 2003, Tkalin et al 1993).
International guidelines, advising the management of dredged material, recommend the
assessment of physical, chemical and biological parameters such as fishes or macrozoobenthic
communities (IMO 2000, OSPAR 2004). Dumping causes physical disturbance, burial of
benthic organisms and a general change in substrate matter, which again may affect these
benthic communities directly.
In the Elbe River altered hydrodynamics reinforced the accumulation of sediment in recent
years (HPA 2005). The city of Hamburg received permission to dump lightly polluted
sediment, characterised as muddy sand containing equal proportions of silt, very fine and fine
sand into the German Bight (Folk 1980). The handling of dredged material and dumping
activity is regulated by German guidelines in respect to London and OSPAR conventions
(BfG 1999, BfG 2009). The actual dumping site measures 400 square metres. Bearing
revealed a three metres high rising at the dumping site containing mainly sandy sediments as
obtained by grain size analyses. Acoustic Doppler Current Profiler (ADCP) analyses recorded
that upon dumping, fine-grained material drifts about eight kilometres until settling down
(HPA 2005). The monitoring program at the dumping site targets among others the
contaminant content of the sediments, the macrozoobenthic community and the fish fauna.
During the dumping period from 2005 to 2010 a significant increase of organic pollutants,
precisely poly aromatic hydrocarbons (PAH) and organotin compounds was reported for the
dumping site. Simultaneously, investigations of the macrozoobenthic communities revealed a
decrease in species richness and density (HPA 2010). Thus far, analyses of bacterial
communities are not implemented in monitoring programs.
Investigating the structure and composition of bacterial communities may be a promising tool
to assess environmental changes within monitoring programs. Bacterial communities are the
most abundant sediment organisms and regulate substantial functions such as nutrient cycling
(Ramette et al 2009). Bacteria also cycle manganese, iron or even toxic metals (Ford and
Ryan 1995). The integration of bacterial communities’ in monitoring programs may allow for
37
a faster and earlier assessment of environmental perturbation than well-established monitoring
tools (such as investigating macrozoobenthos and fish populations).
Several studies have addressed the impact of perturbation on bacterial communities (DeanRoss and Mills 1989, Gillan et al 2005, Roling et al 2001, Wang et al 2011). Bacterial
communities react to physical disturbance, as sieving, with changes in community structure
and reduced biomass (Findlay et al 1990). Observations of the impact of heavy metal or oil
contamination on bacterial communities revealed that the contamination affects the structure
as well as the function of bacterial communities (dos Santos et al 2011, Gremion et al 2004,
Suarez-Suarez et al 2011). The deposition of polluted sediments has been predominantly
investigated in mesocosm experiments (Kan et al 2011, Nayar et al 2004, Toes et al 2008). A
comparison of polluted and non-polluted samples revealed different bacterial communities.
However, the effect of heavy metal contamination on bacterial community structure is not
always distinguishable from other environmental factors in the field (Dean-Ross and Mills
1989, Gillan 2004).
To our knowledge, fine-scale investigations, evaluating the spatial perturbation of dumping
activity on the bacterial community remain lacking. In an interdisciplinary project we initiated
fine-scale investigations of the benthic bacterial community at the dumping site in the
German Bight. The monitoring program itself was designed beforehand according to the
German guidelines for dredged material handling (BfG 1999) and GÜBAK-WSV (BfG
2009). The sampling scheme comprises 125 sampling stations grouped into a priori regions
by distance to the dumping centre (e.g. 1 km, 1.5 km etc), including the dumping and
reference sites. Bacterial community structure was estimated from a direct comparison to this
reference site (12 km north off the dumping site and thus not affected by the dumping
activity). We performed Automated Ribosomal Intergenic Spacer Analysis (ARISA),
combined with ribosomal sequencing of representative samples to investigate bacterial
community structures. Combining biotic information and geochemical data (including
information on grain size fractions, several pollutants, elemental nitrogen, sulphur,
phosphorus and organic carbon) was implemented using multivariate analysis, which is a
feasible tool for predicting the causal factors of bacterial community structures
(Cao et at 2006, Liu et al 2011).
The objectives of this study are as follow: a) to investigate bacterial communities in the a
priori regions via ARISA fingerprinting, b) to compare bacterial community information with
38
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contextual environmental data, and c) to identify community members and structures in
representative samples.
Materials and methods
Site description and sampling
Fig. 1 Location of study site with sampling stations in the German Bight. Ten sampling stations are located at
the immediate dumping centre, 24 others are situated in a range of 1 km. 20 sampling sites are located each at a
distance of 1.5 km, 2 km and 3 km and another 11 are positioned on transects at 6, 9 and 12 km distance. The
reference site consists of 20 sampling stations. The dredging zone is marked with a red star. The 34 sampling
stations until 1 km were pooled as ‘dumping site’ (blue). The sampling stations arranged in circles up to 3km
were grouped as ‘surrounding’ (green). The ‘transects’ are comprising sampling stations until 12 km distance
(yellow) and finally the sampling stations of the ‘reference site’ (red) represent the fourth group.
Table 1 A priori regions, groups and sediment classification after Folk (1980).
Groups
a priori Regions
Sediment
April 2010
August 2010
dumping site
dumping centre (400m*400m)
< 1 km
1 km
1.5 km
2 km
3 km
6 km
9 km
12 km
reference
clayey sand
muddy sand
sandy clay
sandy mud
sandy clay
sandy clay
clayey sand
clayey sand
muddy sand
sandy mud
sand
muddy sand
sandy mud
sandy mud
sandy clay
sandy mud
muddy sand/sandy mud
sandy mud
muddy sand
sandy mud
sand
muddy sand
clayey sand
sandy mud
sandy clay
sandy clay
muddy sand/sandy mud
muddy sand
muddy sand
sandy mud
surrounding
transects
reference
The study site is located in the southern part of the German Bight (54°03Ń 07°58É). Water
depths range between 20 and 35 m. Sediments were classified according to Folk (1980)
39
(Table 1). Sediments at the study site are sandy at the immediate dumping centre, whereas the
reference site consists of sandy mud. Sampling was performed in August 2009, April 2010
and August 2010. Dumping activities were conducted in October 2008 and from October
2009 to February 2010. Each sampling campaign consisted of 125 stations comprising
dumping and a reference sites (Fig. 1). The sampling stations were grouped a priori into
regions. Based on these a priori regions, we further categorised the sampling stations into
four groups for visualisation (Fig. 1, Table 1): ‘Reference site’, ‘transects’, ‘surrounding’ and
‘dumping site’. All sediment samples were collected with a van Veen grab (0.1 m³). On
board, the sediment was poured into a metal box and homogenised. To ensure coherent
analyses, the samples for analyses of the bacterial communities as well as the samples for
physicochemical analyses were taken from this sediment homogenate. For bacterial
community analysis, three subsamples were stored immediately after collection at -20°C in 50
ml falcon tubes.
DNA extraction and quantification
DNA was extracted using the PowerSoil Kit (MoBio Laboratories, Carlsbad, CA, USA)
following the manufacturer’s protocol. Three subsamples of 0.25 g sediment were collected,
and the extracted DNA was eluted in 50 µl elution buffer. Genomic DNA concentrations of
the subsamples were measured by photometry using the Infinite M200 (Tecan Austria GmbH,
Gröding, Austria). DNA was measured in duplicate.
Automated Ribosomal Intergenic Spacer Analysis (ARISA)
The intergenic spacer region (ITS) region of the bacterial genome was amplified with the
primer set S-D-Bact-1522-b-S-20 [5´-TGC GGC TGG ATC CCC TCC TT-3´] and L—DBact-132-a-A-18 [5´-CCG GGT TTC CCC ATT CGG-3´] (Ranjard et al 2000). The forward
primer was labelled with an infrared dye (IRD700). The PCR products of the subsamples
were separated in a 5.5 % polyacrylamide gel prepared following the manufacturer’s protocol
(LI-COR Biosciences, Lincoln, Nebraska, USA).
Ribosomal tag sequencing
Based on significant differences in community structure obtained by ARISA fingerprinting
samples for ribosomal tag sequencing were selected. Genomic DNA from one subsample of
the chosen The tag PCR approach as well as the sequencing approach were performed by
40
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LGC Genomics (Berlin, Germany). The V1-V6 region of the 16S RNA gene was amplified
using the following primer set: forward GM3 5'-AGAGTTTGATCMTGGC-3' and reverse
907R 5'-CCGTCAATTCMTTTGAGTTT-3'. Sequencing was performed in a 454 Roche
Genome Sequencer FLX + Titanium.
OTU definition for ARISA and ribosomal tag sequencing
ARISA fingerprints were all edited by BioNumerics Version 5.1 (Applied Maths NV, SintMartens-Latem, Belgium). Clustering of ARISA-OTUs (operational taxonomic units) (bands)
into classes was performed as previously shown (Kovacs et al 2010). Peaks > 1200 bp were
negligible in the samples. ARISA-OTUs were analysed based on a constructed binary table
(01).
Pyrosequencing data were processed for quality and barcode recovery with MOTHUR
(Version 1.22.0) (Schloss et al 2009). Sequences were clustered at 97 % similarity into 454OTUs. Taxonomic information was obtained in parallel. For LIBSHUFF analysis, singletons
were excluded from the data set using the subroutines split.abund (cutoff=1). Randomly,
6 950 sequences per sample were chosen.
All environmental data (Table 2) were provided by the HPA. The total sediment was analysed
following the HABAK guidelines (BfG 1999).
41
Table 2 Environmental data used in redundancy analysis (RDA) and variance partitioning. For RDA single
values of grain size fractions, S, N, P, C and heavy metals were used; for PAH, PCB, HCH and DDX the sums
of single values respectively. In variance partitioning variables were classified in grain size, S, N, P, C, organic
pollutants (sums of PAH, PCB, HCH, DDX and hydrocarbons) and heavy metals.
Grain size fractions
< 20µm
20-63µm
63-100µm
100-200µm
200-630µm
630-1000µm
1000-2000µm
S, N, P, C
TOC (C)
nitrogen (N)
sulphur (S)
phosphor (P)
Hydrocarbons
Sum Polycyclic Aromatic Hydrocarbons (PAH)
naphthaline
fluorene
phenanthrene
anthracene
fluoranthene
pyrene
benz(a)anthracene
chrysene
benzo(b)fluoranthene
benzo(k)fluoranthene
benzo(a)pyrene
dibenz(ah)anthracene
benzo(ghi)perylene
indeno(1.2.3cd)pyrene
Sum Chlorinated Diphenyls (PCB)
PCB28
PCB52
PCB101
PCB118
PCB138
PCB153
PCB180
42
Sum Hexachlorocyclohexane (HCH)
alphaHCH
betaHCH
gammaHCH
deltaHCH
Sum Dichlorodiphenyldichloroethane (DDT) and metabolites
ppDDE
opDDD
ppDDD
opDDT
ppDDT
Sum Organotin Compounds
monobutyltin (MBT)
dibutyltin (DBT)
tributyltin (TBT)
tetrabutyltin
Heavy Metals
arsenic
lead
cadmium
chrome
copper
nickel
mercury
zinc
CHAPTER II
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Statistics
Univariate Statistics
environmental variables were performed with a Spearman´s rank correlation coefficient. Oneway factorial analysis of variance (ANOVA) was performed to test the effect of the a priori
regions on ARISA-OTUs. Significant factors were then compared using a post hoc HSD test
for unequal group size. All univariate statistical tests were tested at α = 0.05.
Multivariate statistics
For non-metric multidimensional scaling (NMDS) (PRIMER Version 6, PRIMER-E Ltd,
Lutton, UK) (Clarke and Gorley 2006), the Jaccard Index was applied in all cases. Analysis of
similarities (ANOSIM) was employed in pairwise tests to assess the significant differences in
groups of bacterial communities a) at each sampling station (testing similarity of replicates)
and b) among different sites grouped according to their sampling regions (e.g. dumping
centre, reference site, 1 km). The null hypothesises were a) “no differences with regard to
sample position exist” and b) “no differences with regard to sample region exist”. These
analyses resulted in Global R values indicating the degree of separation. Values of p < 0.1
were considered significant.
The examination of relationships between bacterial community patterns and environmental
data was conducted via CANOCO (Version 4.5; Biometris-Plant Research International,
Wageningen, the Netherlands). First, detrended correspondence analysis (DCA) was
performed to test whether linear or unimodal models were the best fit for the ARISA data set
(Lepš and Šmilauer 2003). Redundancy analysis (RDA) was performed to test which
environmental factors (Table 2) explain the significant variation in the bacterial communities.
The data were not transformed prior to the RDA. Factors with a variance inflation factor > 15
were excluded (Legendre and Legendre 1998). The significance of the RDA models and the
selected variables were determined by 499 Monte Carlo permutations at p < 0.05 for each
group. The individual effects of factor groups (grain size; elemental composition, organic
pollutants and heavy metals) on the variation in bacterial communities were further
investigated by variance partitioning (Legendre and Legendre 1998).
43
Geostatistics
The software package ArcGIS Version 10 (ESRI Co, Redlands, CA, USA) was used to show
spatial distributions of the data. Geostatistical analysis using the ordinary kriging subroutine,
mainly the spherical semivariogram model, was performed. Prediction errors, i.e., mean errors
and mean standard errors, were adjusted to near zero. The root mean square error was
adjusted close to 1. Moreover, root mean square and standard errors were highly similar. For
grain size fractions and ARISA-OTUs, all 125 data points could be used; for heavy metals
and organic pollutants, only 52 stations were used.
Phylogenetic Analyses
After sorting and quality control, the total number of OTUs was used for predictive
rarefaction analysis and richness indices (invsimpson, ACE and Chao1). For the actual
analysis rare species (n=1) were excluded. The MOTHUR subroutine LIBSHUFF was used to
investigate significant differences within the whole community structure of the samples. A
significance level of p < 0.05 was applied. The OTUs were subjected to cluster analysis
(PRIMER Version 6, PRIMER-E Ltd, Lutton, UK) (Clarke and Gorley 2006) in order to
investigate their community structure among the sampling sites. Therefore OUT data were log
transformed and the Bray Curtis similarity index applied. Cluster analysis was performed
using the group average.
44
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Results
Geochemical characteristics of the sampling site
All parameters are summarised in Supplementary Table S1. The sampling site displayed
strong grain size and elemental composition gradients that increased from the southwest to the
northeast (Fig. 2).
Fig. 2 Spatial distribution according to ordinary kriging of the fine grain fraction < 20 µm, total organic carbon
(TOC), polycyclic aromatic hydrocarbons (PAH) and organotin compounds (Organotin) in August 2009 (vertical
A; D; G; J), April 2010 (vertical B; E; H; K), August 2010 (vertical C; F; I; L). Dots represent the 125 and 52
sampling stations, respectively.
45
Fine grain fractions (< 20 µm) occurred predominantly in the northeastern region (Fig. 2 A-C;
up to 50 % of the total grain size), whereas only 14 % of the sediment at the dumping centre
harboured < 20 µm grain. The TOC content of the dumping centre was 0.5 % in August 2009
and approximately 0.3 % in April and August 2010 (Fig. 2 D-F). Approximately 1 % TOC
was recorded at the reference site; additionally, high amounts of nitrogen (1000 mg/kg),
sulphur (4000 mg/kg) and phosphorus (400 mg/kg) were detected. We observed lower values
for these elements at the dumping centre. Predominantly nitrogen (166-491 mg/kg) and
sulphur (420-860 mg/kg) content exhibited large differences compared to the stations at the
reference site. Organic pollutants, such as poly aromatic hydrocarbons (PAH), could be
detected at the whole study site. Organotin compounds were detected at the dumping centre at
higher concentrations (79 µg/kg August 2009, 10 µg/kg in April and August 2010), whereas 5
µg/kg of organotin compounds were detected at the reference site (Fig. 2 G-L).
ARISA Fingerprints
Changes in the bacterial community structure in the a priori regions were investigated by
ARISA fingerprinting. Prior to the analysis of the ARISA fingerprints, the similarity among
replicates obtained from the same sampling station was tested indirectly via ANOSIM.
Therefore sampling stations were tested for significant differences. In all cases, the Global R
confirmed significant differences among all sampling stations (Supplementary Table S2).
This result indicated high similarities among replicates. Thus, ARISA fingerprints results are
based on one replicate per station. Figures 3-5 summarise all analyses performed for each
sampling campaign.
We used non-metric multidimensional scaling to display the ARISA fingerprints of all four
groups (‘dumping site’, ‘surrounding’, ‘transects’, ‘reference site’) illustrated in Figure 1
(Fig. 3A-5A). ANOSIM was applied to identify differences in the bacterial communities
(Table 3) between the a priori regions grouped by HPA (Table 1). In all cases, bacterial
communities of the a priori dumping centre and reference site regions were significantly
different (Fig. 3A-5A, Table 3). The non-metric multi-dimensional scaling of ARISA
fingerprints in August 2009 displayed two clear subgroups among bacterial communities from
the groups ‘surrounding’ and ‘reference site’ sampling stations (Fig. 3A).
46
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Table 3 Results of analysis of similarities (ANOSIM) showing the global R of pairwise comparisons of a priori
regions. Significant values bold (p < 0.05).
dumping site
1.5 km
2 km
0.194
0.110
0.098
0.150
-0.054
-0.167
0.100
0.217
0.062
0.790
0.790
0.562
0.078
0.046
-0.176
0.081
0.354
0.643
0.538
0.531
0.591
0.619
0.344
0.214
dumping site
< 1 km
centre
< 1 km
1 km
0.015
0.357
-0.315
surrounding
1 km
centre
< 1 km
1 km
0.61
0.61
0.03
surrounding
centre
1.5 km
2 km
3 km
0.783
0.505
0.245
6 km
9 km
12 km
reference
1.5 km
2 km
3 km
0.72
0.86
0.54
0.28
0.16
0.25
6 km
9 km
12 km
0.73
0.80
0.80
reference
transects
3 km
6 km
9 km
0.247
0.216
0.186
0.021
-0.074
-0.127
0.125
0.036
-0.036
0.442
0.286
0.127
0.390
0.271
0.01
0.34
-0.15
0.30
0.05
0.26
0.12
0.14
0.25
0.32
0.17
0.33
0.12
0.37
0.32
0.40
0.51
0.52
-0.11
0.16
0.01
0.20
-0.04
-0.24
0.80
0.50
0.39
0.36
0.55
0.34
0.12
0.36
dumping site
Region
surrounding
centre
< 1 km
1 km
0.68
0.75
0.50
surrounding
dumping site
1.5 km
2 km
3 km
0.94
0.84
0.45
0.64
0.39
0.40
-0.06
0.05
-0.18
0.09
0.10
0.04
6 km
9 km
12 km
0.77
0.75
0.46
0.11
0.42
0.40
0.20
-0.02
1.00
0.35
0.47
0.88
-0.07
0.20
0.62
-0.18
-0.07
0.18
-0.11
0.25
0.14
reference
0.85
0.65
0.12
0.38
0.25
0.18
0.17
0.32
Reference
12 km
reference
transects
August 2009
0.333
transects
April 2010
-0.26
transects
August 2010
0.68
47
Fig. 3 Sampling campaign August 2009. A Non-metric multidimensional scaling (NMDS) plot of the Automated
Ribosomal Intergenic Spacer Analysis (ARISA) profiles based on the Jaccard Index. Each square represents a
profile of a sampling station belonging to the group ‘dumping site’ (blue), ‘surrounding’ (green), ‘transects’
(yellow), ‘reference site’ (red). B Partitioning of bacterial variation (%) into the relative effects of contextual
factor groups as determined by 499 Monte Carlo permutations. C Redundancy analysis (RDA) biplot of bacterial
communities and contextual parameters. Squares represent ARISA profiles colourised reffering to their
associated group (see A). Significant environmental factors are displayed in red. D Spatial distribution of the
sum of ARISA-OTUs of each sampling station as calculated by ordinary kriging. Dots represent the 125
sampling stations.
The bacterial community structure of samples obtained at the ‘dumping site’, more precisely a
priori centre and < 1 km, did not differ significantly in August 2009 (Table 3). In April and
August 2010, we observed significant differences comparing the structure of these bacterial
communities at the ‘dumping site’ (Fig. 4A and 5A, Table 3).
The alpha diversity, as estimated by ARISA-OTU numbers, was analysed by ordinary kriging
and analysis of variance in respect to corresponding a priori regions (Table 1). Generally
highest ARISA-OTU numbers were recorded in August 2009 and 2010 (22-107 OTUs;
Fig. 3D and 5D), with significantly higher ARISA-OTU numbers in the a priori region 1.5
km when compared with a priori regions < 1 km and reference (p < 0.001, Fig. 3D and 5D).
In April 2010, ARISA-OTUs ranged from 12 to 81 ARISA-OTUs at the different sampling
48
CHAPTER II
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Fig.4 Sampling campaign April 2010. A Non-metric multidimensional scaling (NMDS) plot of the Automated
Ribosomal Intergenic Spacer Analysis profiles based on the Jaccard Index. Each square represents a profile of a
sampling station belonging to the group ‘dumping site’ (blue), ‘surrounding’ (green), ‘transects’ (yellow),
‘reference site’ (red). B Partitioning of bacterial variation into the relative effects of contextual factor groups as
determined by 499 Monte Carlo permutations. C Redundancy analysis (RDA) biplot of bacterial communities
and contextual parameters. Squares represent Automated Ribosomal Intergenic Spacer Analysis profiles
colourised reffering to their associated group: ‘dumping site’ (blue), ‘surrounding’ (green), ‘transects’ (yellow),
‘reference site’ (red). Significant environmental factors are displayed in red. D Spatial distribution of the sum of
ARISA-OTUs of each sampling station as calculated by ordinary kriging. Dots represent the 125 sampling
stations.
positions (Fig. 4D). ARISA-OTU numbers at the a priori reference were significantly
(p < 0.001) lower compared with the a priori regions dumping centre, 1.5 km and 3 km.
Relation to environmental data
Prior to the analysis environmental factors were investigated for correlation in order to
consider these for the interpretation of results obtained via redundancy analysis. The
Spearman’s rank correlation revealed significant correlations among the fine grain size
fractions, organic carbon, sulphur, phosphorus and nitrogen content and heavy metals, such as
49
Fig. 5 Sampling campaign August 2010. A Non-metric multidimensional scaling (NMDS) plot of the Automated
Ribosomal Intergenic Spacer Analysis profiles based on the Jaccard Index. Each square represents a profile of a
sampling station belonging to the group ‘dumping site’ (blue), ‘surrounding’ (green), ‘transects’ (yellow),
‘reference site’ (red). B Partitioning of bacterial variation into the relative effects of contextual factor groups as
determined by 499 Monte Carlo permutations. C Redundancy analysis (RDA) biplot of bacterial communities
and contextual parameters. Squares represent Automated Ribosomal Intergenic Spacer Analysis profiles
colourised reffering to their associated group: ‘dumping site’ (blue), ‘surrounding’ (green), ‘transects’ (yellow),
‘reference site’ (red). Significant environmental factors are displayed in red. D Spatial distribution of the sum of
ARISA-OTUs of each sampling station as calculated by ordinary kriging. Dots represent the 125 sampling
stations.
arsenic, lead, chrome, copper, nickel and zinc, for all sampling campaigns. Additionally,
DDX sums correlated with the sums of HCH, PCB and organotin compounds.
We aimed to investigate the relationship between bacterial community structures as obtained
via ARISA fingerprinting and simultaneously recorded environmental factors in redundancy
analyses. Environmental parameters (Table 2) were recorded at 52 out of 125 sampling sites
(Supplementary S3). A detrended correspondence analysis, as well as a redundancy analysis
based on these data and the corresponding ARISA fingerprints, was performed.
A gradient length of < 2.5 for all first axes of the detrended correspondence analysis
suggested a linear model, such as redundancy analysis, as the best method for analysing the
data sets.
50
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The first two axes of the redundancy explained between 14-17 % of the total variation
(Supplementary S4). The first axis of the redundancy analysis of the data sets from August
2009 and April 2010 was associated with larger grain size fractions and heavy metals such as
mercury, copper and zinc. The second axis was determined by a gradient formed by organic
pollutants and fine grain fractions associated with sulphur, nitrogen, phosphorus, organic
carbon and heavy metals such as chrome and arsenic. These axes were inverted for the data
set from August 2010. Factors omitted from the analysis are shown in Table 4. Bacterial
communities of the group ‘reference site’ correlated with larger grain sizes, whereas
communities of the group ‘dumping site’ correlated with organic pollutants (Fig. 3C, 4C
and 5C). Organotin compounds exhibited significant conditional effects in all analyses
(Table 4). The respective effects of each factor group were disentangled by variance
partitioning analysis (Fig. 3D, 4D and 5D). The model was based on the complete data set
(n=52). The environmental parameters were grouped according to grain size (< 20 µm, 20 63 µm, 63 - 100 µm, 100 - 200 µm, 200 - 630 µm, 630 - 1000 µm, 1000 - 2000 µm); organic
pollutants (ΣPCB, ΣDDX, ΣHCH, Σorganotin compounds and Σhydrocarbons); S, N, P, C
(sulphur, nitrogen, phosphorus, organic carbon) and heavy metals (arsenic, lead, cadmium,
chrome, copper, nickel, mercury, zinc). Partitioning the variance of bacterial communities
revealed that the highest proportion of variance was explained by organic pollutants and
heavy metals in April and August 2010, while grain size explained a higher proportion as
compared to heavy metals in August 2009 (Fig. 3-5B).
Phylogenetic- and 454-OTU-based analyses
The NMDS plot of ARISA profiles in August 2009 revealed subgroups of bacterial
communities of the groups ‘surrounding’ and ‘reference site’. According to these subgroups,
ANOSIM results suggested a high variability within the data set. For ribosomal tag
sequencing, we chose one sample from the dumping centre, five from the ‘surrounding’, two
from the ‘reference site’ (reference site 1 and reference site 2) and one sample from the
dredging zone in the Elbe River (Supplementary S5).
In total, 669 647 sequences were retrieved from ribosomal tag sequencing, and 24 611 OTUs
at a similarity level of 0.97 were detected. Rarefaction curves revealed similar profiles, which
started to become asymptotic in all cases (Supplementary S6). We observed the highest
richness for communities from the reference site and the lowest richness from the dumping
centre (Supplementary S6).
51
Table 4. Conditional effects of forwardly selected environmental variables and variance inflation factor of
excluded parameters as determined by RDA.
August 2009
Environmental variable
April 2010
Lambda-A
F ratio
0.05
0.03
0.03
0.03
0.02
0.02
0.02
0.03
0.02
0.03
0.02
0.02
0.02
0.02
0.02
0.01
0.02
0.02
0.02
2.90**
1.53NS
1.38NS
1.5NS
1.24NS
1.24NS
1.25NS
1.16NS
1.65*
1.26NS
1.17NS
1.18NS
1.13NS
1.1NS
1.18NS
1.01NS
1.10NS
1.03NS
0.84NS
Lambda-A
F-ratio
Sum organotin compounds
20 - 63 µm
nickel
nitrogen
<20 µm
copper
63 - 100 µm
arsenic
1000 - 2000 µm
630 - 1000 µm
Sum PAH
Sum DDX
0.06
0.04
0.03
0.03
0.03
0.02
0.02
0.02
0.02
0.02
0.02
0.02
2.98**
1.81**
1.52*
1.49*
1.43*
1.1NS
1.04NS
0.98NS
1NS
1.02NS
0.96NS
1.09NS
Sum PAH
mercury
cadmium
chrome
phosphor
hydrocarbons
Sum HCH
TOC VIF >15
100-200µm VIF >15
200-630µm VIF >15
sulphur VIF >15
lead VIF >15
zinc VIF >15
0.02
0.03
0.02
0.01
0.02
0.01
0.01
1.21NS
1.15NS
0.97NS
0.84NS
0.76NS
0.68NS
0.71NS
100-200 µm
Sum PAH
TOC
20-63 µm
1000-2000 µm
copper
Sum DDX
200-630 µm
Sum PCB
phosphor
630-1000 µm
Sum HCH
hydrocarbons
chrome
cadmium
mercury
nitrogen
sulfur
20µm VIF >15
63-100µm VIF >15
arsenic VIF >15
lead VIF >15
nickel VIF >15
zinc VIF >15
August 2010
Sum HCH
copper
20 - 63 µm
chrome
mercury
zinc
< 20 µm
1000 - 2000 µm
630 - 1000 µm
arsenic
nitrogen
TOC
Sum PAH
lead
63 - 100 µm
hydrocarabons
Sum PCB
TOC VIF >15
100-200µm VIF >15
sulphur VIF >15
phosphor VIF >15
Sum DDX VIF >15
cadmium VIF >15
nickel VIF >15
Lambda-A
F-ratio
0.06
0.03
0.02
0.04
0.04
0.03
0.02
0.02
0.02
0.03
0.02
0.02
0.02
0.01
0.02
0.02
0.01
0.01
2.99**
1.56*
1.44*
2.06**
1.82**
1.78**
1.49NS
1.18NS
1.18NS
1.45NS
1.25NS
1.18NS
0.98NS
1NS
0.93NS
0.94NS
0.82NS
0.77NS
Lambda-A represents the variance each variable explains in the model.Statistical significance is indicated by **
(p < 0.01), * (p <0.05), and NS (not significant) as determined by 499 Monte Carlo permutations.
52
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We were interested in investigating solely abundant bacterial groups for differences regarding
their community composition, consequently rare species were omitted. After removing
singeltons (n=1) from the data set we observed 5627 OTUs which remained for the analysis.
Lowest OTU numbers (~ 1000 OTUs) were detected in the Elbe and highest OTU numbers at
the reference site (~ 2200 OTUs, Fig. 6A). In total, 16 phyla were observed (Fig. 6B). In all
cases, sequences related to Proteobacteria dominated the samples (Fig. 6B). Highest
sequence numbers (~ 8500 sequences) were observed for the Elbe (Fig. 6B), contrary lowest
sequence numbers were detected at the reference site (~ 3000 sequences). LIBSHUFF
analyses revealed significant differences (p < 0.0001) in the bacterial community structure
from Elbe and dumping centre as compared to all the others. Additionally, the reference site
differed in bacterial community structure compared to surrounding 3 and reference 1 to
surrounding 1. Subsequently we aimed to investigate differences among sampling sites
regarding the most frequent phyla Proteobacteria and Bacteroidetes. In all cases dumping
centre and Elbe shared highest similarities. Alpha- and Betaproteobacteria were detected only
in considerable numbers in the Elbe and at the dumping centre (Fig. 6C and 6D). Whereby
Rhizobiales, Hypomicrobium and Methylocystaceae from the Alphaproteobacteria; and
Burkholeriales and Hydrogenophilaceae from the Betaproteobacteria were observed in both
samples. The class of Deltaproteobacteria contained generally high sequence numbers for the
marine sites (Fig. 6E). Fewest sequences affiliated to Deltaproteobacteria were reported for
the Elbe (~ 700 sequences). The reference sites had only few sequences affiliated to
Deltaproteobacteria (reference 1: ~ 1600, reference 2: ~ 1900) as compared to dumping
centre (~ 3200 sequences) and surrounding (~ 2300 sequences, Fig. 6E). The highest diversity
however was observed in the Elbe, comprising 14 bacterial groups within the
Deltaproteobacteria. The marine samples were dominated by Desulfobulbaceae and
Desulfuromonadaceae. However, considerably higher sequence numbers were detected for
Desulfuromonadaceae at the dumping centre when compared to all other sites (Fig. 6E).
Unfortunately, Gammaproteobacteria comprised mainly unclassified sequences (Fig. 6F).
Investigating the phylum Bacteroidetes we recorded exclusively sequences affiliated to the
Flavobacteria at the marine sites (Fig. 6G). The Elbe contained sequences affiliated to
Porphyromonadaceae, Flavobacteriaceae, Chitinophagaceae and Sphingobacterales. Few
sequences affiliated to Porphyromonadaceae, Chitinophagaceae, Saprospiraceae and
Sphingobacterales were detected at the dumping centre (Fig. 6H).
53
Fig. 6 Phylogenetic classification for the ribosomal tag sequencing results obtained by MOTHUR of nine
representative samples based on OTUs (0.97) omitting singletons (n > 1). A total numbers of OTUs detected in
the samples, B Stacked bars and cluster analysis on phylum level based on observed OTUs C
Alphaproteobacteria, D Betaproteobacteria, E Deltaproteobacteria, F Epsilonproteobacteria, G
Flavobacteriales, H Bacteroidales and Sphingobacteriales.
54
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Discussion
Investigations of dumping activities as stated by the OSPAR report draw the following
consequences resulting from dumping activities: the increase of contaminants, a general
change in substrate matter which may affect benthic communities directly, physical
disturbance and burial of benthic organisms and the intrusion of foreign species (OSPAR
2004). Our results clearly confirm that changes in substrate matter as well as physical
disturbance affected benthic bacterial community’s structure. Additionally we showed that
not only the dredged freshwater sediment but also typical freshwater bacteria were observed
at the dumping centre even ten months after a dumping activity.
Changes in substrate matter
The monitoring design grouped sampling stations by distance into a priori regions (e.g.
dumping centre, 1 km, 1.5km etc). We did not find any specific structures of bacterial
communities (ARISA fingerprinting) referring to these a priori regions. Solely significant
differences obtained between bacterial communities from the dumping centre and reference
were observed in all sampling campaigns. The observation of a fundamentally different
granular structure at the dumping centre (clayey sand – sand) as compared to the reference
site (sandy mud) combined with lowest values for carbon, nitrogen, phosphorus and sulphur
at the dumping centre leads to the assumption that these fundamentally different conditions
might explain the different bacterial communities in these regions. Grain size distribution, in
addition to other physicochemical factors, represents the main driving factor influencing
bacterial communities (Dale 1974, DeFlaun and Mayer 1983). Sandy sediments harbour
different bacterial groups than muddy sediments (Llobet-Brossa et al 1998). The sandy
texture of the dumping centre contains, in comparison to the reference site, a low TOC and
low sulphur, nitrogen and phosphorus content. Moreover, an increase of organotin and poly
aromatic compounds in comparison to the reference site was reported (HPA 2005, HPA 2006,
HPA 2007, HPA 2008, HPA 2009, HPA 2010). Other studies have indicated a relationship
between pollutant load in sediments and bacterial communities (Edlund et al 2006, Gremion
et al 2004, Vishnivetskaya et al 2011, Zhang et al 2008). The impact of dredging on bacterial
communities was investigated by Edlund and Jansson (2006). They reported a shift in
community structure and composition before and after the intrusion in the dredging area and
concluded that the pollutant load resulted in a change in the bacterial community (Edlund and
Jansson 2006). We observed a strong gradient formed by sediment grain size fractions and
organic pollutants in all redundancy analyses (Fig. 3-5). Organotin compounds had always a
55
significant conditional effect. The gradient formed by the grain size fractions confirms our
hypothesis that the geochemical conditions of the sediments are shaping the bacterial
communities predominantly. However, the significant conditional effect of organotin
compounds must be interpreted with caution. Our results show, that organotin compounds are
correlated with ΣHCH, ΣPCB and ΣDDX. The distribution of organotin in the sediment,
however, is rather heterogeneous because organotin compounds most likely reside as paint
flakes in the sediment (Dowson et al 1993, Hoch 2001). A causal relationship between the
metabolism of bacteria and the occurrence of organotin compounds cannot be determined.
Moreover, a strong relationship among fine-grained sediments (< 20 µm and 20-63 µm),
elemental composition and several heavy metals, including arsenic, lead, chrome and nickel,
was observed in all of the redundancy analyses. Other studies have revealed strong
interactions between fine-grained sediments, nutrients and contaminants (Owens et al 2005),
too. This strong correlation hinders the evaluation of single effects on bacterial community
variation.
Variance partitioning (Fig. 3B-5B) was performed to assess the influence of grain size,
elemental composition, organic pollutants and heavy metals. The results suggest, consistent
with our previous hypothesis, the existence of a strong gradient formed by grain size
distribution and probably some organic pollutants. Variance partitioning revealed a complex
framework between grain size, elemental composition, organic pollutants and heavy metals. It
seems that the variability of bacterial communities cannot be assigned to a single factor or
factor group. Thus, the combined effects explain more of the variance in the community
structure than each group individually. Already other field studies failed in assigning changes
in community structure to single factors in the field. Dean-Ross and co-workers (1989) as
well as Gillian (2005) stated difficulties in distinguishing the impact of heavy metal pollution
from other factors influencing bacterial community structure. One possible approach to
overcome this problem in the future could be the linkage of laboratory experiments and field
studies. In laboratory experiments single factors can be manipulated and observed in a
controlled design. The results again can be linked to observations in the field in order to better
estimate the true pollution impact.
Physical disturbance
An interesting finding of our study was the formation of significant different bacterial
community structures at the dumping site in 2010 while these communities were rather
similar in our sampling campaign in 2009 (Table 3). We hypothesise that the dumping
56
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activity between the sampling campaigns of August 2009 and April 2010 led to the recorded
bacterial community shift at the ‘dumping site’. We observed a similar sediment texture at the
‘dumping site’ in 2009 (Table 1) but considerably higher sand proportions at the dumping
centre in 2010. Due to transport and sedimentation processes, fine-grained material composed
of biogenous and terrigenous particles accumulated in the undisturbed phase between the last
dumping activity in October 2008 and our first sampling campaign in August 2009 at the
centre. The dumping activity in 2010 led to a perturbation of the sediment. During the
dumping process, sandy particles accumulate at the dumping centre, whereas fine-grained
material spreads over a distance of up to 8 km (HPA 2005).
In our sampling campaigns 2010 we observed a higher alpha diversity at the dumping centre,
as revealed by ARISA fingerprinting. Several studies dealing with the impact of perturbation
on bacterial communities observed changes to the bacterial community structure. Generally,
the communities respond to disturbance by decreasing community and functional diversity
(Atlas et al 1991, Girvan et al 2005). In the present study, we observed a low alpha diversity
at the dumping site as revealed by ARISA fingerprinting as well as ribosomal tag sequencing
for bacterial communities in 2009, ten months after a dumping activity. Interestingly, two and
six months after a dumping activity, as observed in 2010, the alpha diversity was higher at the
dumping centre. Possibly, freshwater bacteria enter the marine system and survive for several
months at the dumping site but vanish on a longer time scale. This may then in turn result in a
lower alpha diversity at the dumping centre as observed for 2009. Contrary to the sequencing
approach ARISA fingerprinting suggested a low alpha diversity for both the reference site and
dumping centre, too. ARISA fingerprinting is known to possibly underestimate diversity since
unrelated organisms may possess spacer regions of identical length (Fisher and Triplett 1999,
Kovacs et al 2010). Certainly, the ribosomal tag sequencing approach is more accurate then
the ARISA fingerprinting. The sequencing approach confirmed a low alpha diversity at the
dumping centre. Contrary, diversity of the samples from the reference site was high (Fig. 6).
Our sequencing results suggest that the diversity in samples of the reference site is most likely
due to various rare species, here OTUs comprising only few sequences (Fig. 6A and 6B).
Probably these rare species were not covered by the ARISA fingerprinting approach. To date
several studies applying tag sequencing are distinguishing rare from abundant species and
conclude possibly two sub communities (rare biosphere) (Galand et al 2009, Sogin et al
2006). Finally we suppose, concluding from our findings obtained by fingerprinting and
sequencing that the dumping activity led to a less diverse bacterial community at the dumping
site on the long term.
57
Intrusion of freshwater bacteria at the dumping centre
We identified fundamental differences in community structure and composition between
fluvial and marine samples. The bacterial community of the fluvial sample represents a
typical freshwater sediment community (Miskin et al 1999, Zwart et al 2002). Typical groups
such as Betaproteobacteria or Verrucomicrobia were detected. The marine samples were
dominated by Proteobacteria and Bacteroidetes. Thus far, bacterial communities of the
sublittoral shelf sediments in the German Bight are poorly characterised. Studies conducted in
coastal areas such as the Wadden Sea revealed the Planctomycetes, Gammaproteobacteria
and Cytophaga-Flavobacterium cluster. Members of sulphate-reducing Deltaproteobacteria
were predominant, whereas Alphaproteobacteria were only observed in low numbers (LlobetBrossa et al 1998, Musat et al 2006). Antarctic shelf sediment revealed high numbers of
Gamma- and Deltaproteobacteria (Bowman and McCuaig 2003).
Principally, two findings can be drawn from the presented results: Firstly, even ten month
after a dumping activity, typical freshwater bacteria such as Rhizobiales, Hypomicrobium and
Methylocystaceae or Burkholeriales and Hydrogenophilaceae were detected in low numbers
at the dumping centre. This finding might point to a successful establishment or long
persistence of foreign bacterial groups at the dumping centre. Secondly, we observed highest
abundances of Desulfuromonadaceae and Flavobacteriaceae. In the present study,
Deltaproteobacteria dominated all marine samples. This observation was expected since this
group inhabits anoxic environments (Jorgensen 1977, Kondo et al 2007, Mußmann et al
2005). The main proportion of shelf sediments is anoxic, where only the top millimetres are
penetrated by oxygen (Schulz and Zabel 2006). We used a van Veen grab for sampling which
penetrates the sediment up to 30 cm and contains therefore a main proportion of the anoxic
sediment body. Less abundant but still considerable was the skewed distribution of
Bacteroidetes, more precisely Flavobacteriaceae. This group comprises members featuring
various physiological capabilities, furthermore they are adapted to a broad range of
environmental conditions (Weller et al 2000). Generally, Bacteroidetes are strongly
associated with the water column and marine aggregates. However, some studies described
their presence for aerobic and anaerobic sediments, too (Llobet-Brossa et al 1998,
Ravenschlag et al 2001). Flavobacteria are believed to play a pivotal role in degrading
organic matter since they own hydrolytic capabilities (Abell and Bowman 2005, Cottrell
2000). Nowadays Flavobacteriaceae are from great interest in the context of remediation of
organic pollution. It was highlighted that the addition of complex organic substrates resulted
58
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in the growth of Bacteroidetes in anaerobic sediments (Rosselló-Mora et al 1999). In our
study Flavobacteriaceae were observed in all samples, interestingly, at the dumping centre
five times more sequences affiliated to Flavobacteriaceae were detected as compared to all
other marine sites.
Both families, Desulfuromonadaceae and Flavobacteriaceae were already investigated in the
context of environmental pollution. Recently, the response of sulphate-reducing bacteria to an
artificial oil-spill was investigated in a mesocosm study by Suarez-Suarez (2011). The
bacterial community from a pristine environment was exposed to increasing naphthalene and
crude oil contents of up to 0.03 mg/kg. Desulfuromonadaceae and Desulfobulbaceae
dominated oil and naphthalene treatments after incubation. Bissett and co-workers examined
increasing numbers of Flavobacteria and community shifts within this group under regular
inputs of highly labile organic carbon. They conclude that Flavobacteria may play an
important role in the initial degradation of organic matter due to their positive response to
organic pollution (Bissett et al 2008).
High PAH concentrations at the dumping centre may have led to an increase of
Desulfuromonadaceae and Flavobacteriaceae. In our study, we detected naphthalene
concentrations of approximately 0.2 mg/kg at the dumping centre. Additionally, poly aromatic
hydrocarbon (PAH) concentrations of 0.96 mg/kg were recorded at the dumping centre and in
contrast ~ 0.4 mg/kg at the reference site. High PAH concentrations in the whole study area
are likely caused by intensive dumping activity, shipping traffic and riverine input in the past
century.
We showed that the community composition of essential bacterial groups differed at the
dumping centre, suggesting that the dumping resulted in functional changes in the ecosystem.
To further elucidate the consequences of dumping, more information about the interactions of
these bacterial groups in the sediments of the German Bight is urgently needed.
Applicability in monitoring programs
This study aimed to assess the applicability of bacterial community analyses in beforehand
designed monitoring schemes. We showed similar results for bacterial community response
compared to the response of the macrozoobenthos. Both groups of organisms responded with
a decrease of species richness at the immediate dumping centre. This finding itself
demonstrates the capacity of bacterial community investigations for monitoring programs. A
major obstacle of bacterial community analysis, however, is the great variability and diversity
59
within bacterial communities. We recommend for future monitoring programs to integrate
investigations of the diversity as well as composition of bacterial communities in comparison
to a reference and optimally to communities at the dumping site before dumping activities
take place. Diversity measures are still an index for the “fitness” of ecosystems. Additionally,
investigations of the community composition might resolve changes in the communities and
therefore possible responses to environmental pollution and intrusion of foreign communities.
The identification of environmental factors, influencing bacterial communities remains
delicate. Strong correlations of pollutants with grain size fractions of the sediment or nutrients
hinder an accurate analysis. As already mentioned above a combination of laboratory studies
and field observations might be a wise elaboration. Additionally information about the redox
potential or other physicochemical parameters such as temperature, oxygen penetration or pH
might be helpful to capture the complexity of the disturbed benthos.
In conclusion, our study provides for the first time fine-scaled spatial information about
bacterial community structure under the influence of dumped polluted material. Bacterial
community structure and diversity were affected even by lightly polluted material and
ongoing dumping activity. This assumption is based on significant differences between
bacterial community structure and alpha diversity at dumping centre and reference site in all
sampling campaigns. Our correlation and redundancy analyses confirmed the high complexity
of the underlying processes in the benthos. Single factors influencing the bacterial
communities could not be identified adequately. Considering these analyses for monitoring
programs further elaboration of these multivariate analyses is needed. However, we detected a
unique bacterial community at the dumping centre composed of probably specialised marine
groups and freshwater bacteria. These results significantly broaden the knowledge of how
bacterial communities respond to dumping activities.
Acknowledgements
This project was funded by the Hamburg Port Authority (HPA), Bundesanstalt für
Gewässerkunde (BfG), Landesamt für Landwirtschaft, Umwelt und ländliche Räume des
Landes Schleswig-Holstein (LLUR) and Nds. Landesbetrieb für Wasserwirtschaft, Küstenund Naturschutz (NLWKN). We thank our project partners for financial and data support and
for critical discussion of the results in this study. We are grateful for the support of Dr. Jörg
Peplies sharing his knowledge on sequencing data
60
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CHAPTER III
Impact of ocean dumping on bacterial communities
II: GeoChip-based analysis of bacterial communities at a dumping site
a
Corresponding author: rebecca.stoermer@awi.de, phone: (0049)4725/819-3233, fax:
(0049)4725/819-3283
61
Abstract
In between the years 2005 to 2010 approximately 6 000 000 cubic metres sediment was
dumped 15 kilometres south off the island Helgoland in the German Bight (North Sea). The
accompanying monitoring program reported a decrease of macrozoobenthic species richness
and density at the dumping centre. In a pilot study we complemented the monitoring program
by analyses of the benthic bacterial community using functional gene arrays. We applied
analysis of variance and hierarchical clustering to investigate differences between sampling
sites. The relationship between functional genes and environmental factors was disentangled
by distance-based multivariate multiple regression. The bacterial community at the dumping
centre displayed significantly lower gene numbers compared to a reference site. Hierarchical
clustering displayed distinct cluster for samples from Elbe River, dumping site and reference
site. Conclusively, the dumping activity changed persistently the geochemical conditions of
the area resulting in a less diverse bacterial community at the dumping centre.
Keywords: dredged sediment / pollution / multivariate statistics / functional gene arrays
62
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Introduction
Estuaries represent economically valuable areas, constantly evolving and facing a wide range
of natural and human-induced stresses. Worldwide ports and rivers located in estuaries suffer
from high siltation rates caused by erosion and sedimentation. In addition the expansion of
global trade requires increasingly large container ships and thus the constant deepening of
waterways. Inevitably dredging procedures ensure therefore navigation in these areas (de Nijs
et al 2009, McLoughlin 2000, Tanner et al 2000) and most likely the amount of dredged
material will increase in the future (OSPAR 2000). Although most dredged material is
uncontaminated; in some cases the application of major environmental constraints is required
for contaminated material (IMO 2000, OSPAR 2004). International conventions, such as the
London convention, regulate dumping activities in marine areas worldwide (Organization
2000). Additionally, regional conventions exist (OSPAR 2004). Guidelines for the
management of dredged material recommend the assessment of physical, chemical and
biological parameters of both dredged sediment and the dumping sites in order to estimate the
impact of the disposal (OSPAR 2004, IMO 2000). Biological investigations focus in general
on higher organisms such as fishes and macrozoobenthos and additionally, ecotoxicological
assessments are frequently carried out. However, the execution of these directives depend on
national politics of signatory countries (Bartels 2000). Recently, the OSPAR commission
claims to invest more effort in investigating biological responses to the disposal of dredged
material (OSPAR 2009).
The economic history of the Elbe River (Germany) goes back to the 12th century when the
city of Hamburg received trade privileges. Today, the Elbe River and the port of Hamburg
belong to the most important global trade routes. In the past years the amount of dredged
material from the Hamburg port area increased. Already relocated sediment re-accumulates in
the same water system and requires therefore multiple inconclusive dredging processes
(HPA 2005). As a consequence the city of Hamburg applied for permission to dump lightly
polluted river sediment at a dumping site in the German Bight. Hence, in between the years
2005 and 2010 approximately 6 000 000 cubic metres sediment were removed from the Elbe
River near the port area of Hamburg and were dumped at the prescribed site. German
guidelines for the handling of dredged material regulate the dumping activity and base
predominantly on London and OSPAR conventions (BfG 1999, BfG 2009). The dumping site
measures 400 square metres. Recent bearing showed a three metres high rising at the dumping
site consisting of sandy sediments as assessed by grain size analyses. Acoustic Doppler
63
Current Profiler (ADCP) analyses revealed that fine-grained material drifts about eight
kilometres until settling down on the seafloor (HPA 2005). The monitoring of the dumping
site targets, among others, the respective contaminant content of the sediments, the
macrozoobenthos and the fish fauna. During the dumping period from 2005 to 2010 a
significant increase of organic pollutants, precisely poly aromatic hydrocarbons (PAH) and
organotin compounds was reported by the Hamburg Port Authority (HPA). Simultaneously,
investigations of the macrozoobenthos revealed a decrease in species richness and density
(HPA 2010).
In fact dumping activity causes multiple implications. Beside the increase of contaminants,
dumping causes physical disturbance, burial of benthic organisms and a general change in
substrate matter, which again may affect benthic communities directly (OSPAR 2009).
Microbenthic communities (including bacteria) are currently disregarded by prescribed
guidelines for dredged material handling. It is known that physical and chemical perturbation
lead to changes in bacterial community structure and function (dos Santos et al 2011, Findlay
et al 1990, Suarez-Suarez et al 2011). Against this background it appears obvious that
microbenthic communities will be affected by dumping activities just like the
macrozoobenthos. The response of microbenthic communities, as being far more complex
than the macrozoobenthos, is expected to be as complex as the communities themselves.
Today, molecular approaches allow the assessment of microbenthic community’s
information. Therefore, it might be worth considering these approaches in future guidelines.
In an interdisciplinary project we initiated fine-scale investigations of benthic bacterial
communities at the prescribed dumping site in the German Bight. The monitoring itself was
designed beforehand according to the German guidelines for dredged material handling (BfG
1999) and GÜBAK-WSV (BfG 2009). It comprises 125 sampling stations including the
dumping and a reference site. Our first sampling campaign was conducted ten months after a
dumping activity in 2009 (Störmer et al 2012). Bacterial community structure, derived from
16S ribosomal gene analyses, displayed significant differences comparing dumping and
reference sites (Störmer et al 2012). This study assumed that the dumping activity led to
different bacterial communities and a lower alpha diversity at the dumping centre (Störmer et
al 2012). However, information of the functional structure of these communities is still
lacking.
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In the past years functional gene arrays were applied in various environmental studies (He et
al 2007, He et al 2010, Liu et al 2010, Wang et al 2009, Ward et al 2007, Wu et al 2008,
Yergeau et al 2007, Zhou 2003) including heavily contaminated habitats (Lu et al 2012,
Neufeld et al 2006, Van Nostrand et al 2009, Xie et al 2011). Nostrand and co-workers
(2009) found an increase in diversity and overall gene numbers going along with the
stimulation of uranium remediation by ethanol additions in an uranium contaminated aquifer
(Van Nostrand et al 2009). Waldron and co-workers investigated a gradient of contaminant
levels in groundwater. They observed that contamination affects functional gene diversity
(e.g. reduced diversity) and heterogeneity (Waldron et al 2009). Only recently the GeoChip
gene array was implemented in a study investigating microbial community response to the
Deepwater Horizon oil spill. Lu and co-workers found a high enrichment of metabolic genes
especially involved in hydrocarbon degradation in the plume (Lu et al 2012).
Here, we aimed to reveal the functional gene diversity of nine representative samples obtained
in connection with the monitoring program in the dumping region in 2009 by using GeoChip
4.2 (Lu et al 2012). The functional gene array contains probes targeting among others the
gene categories: carbon cycling, nitrogen cycling, and heavy metal resistance.The present
study targets a) the diversity of functional genes and b) environmental factors influencing the
functional gene structure in the bacterial community.
65
Material and methods
Site description and sampling
Fig. 1 Sampling scheme of the dumping site in the German Bight (54°03Ń 07°58É). Samples for GeoChip
analyses are represented as red stars. One sample was taken at the dumping centre, five originate from the
surrounding (1.5km, 2km_1, 2km_2, 3km_1, 3km_2) off the centre and two were chosen from the reference
(reference_1, reference_2). Additionally one sample from the Elbe River (53°32' N 9°56' E) was chosen.
Table 1 Sediment characterisation of the samples after Folk (1980).
Samples
Sediment
Elbe
dumping centre
1.5km
2km_1
2km_2
3km_1
3km_2
reference_1
reference_2
muddy sand
66
clayey sand
sandy mud
sandy clay
sandy clay
sandy clay
sandy clay
sandy mud
sandy mud
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The dumping site is located in the southern part of the German Bight (54°03Ń 07°58É)
15 kilometres south off the island of Helgoland. The current at the dumping site is cyclonic
and influenced by east wind forcing (Staneva et al 2009) and the discharge of the adjacent
rivers (Howarth 2001). Water depths range between 20 and 35 metres. Sediments of the
dumping site are sandy whereas the reference consists of sandy mud (Table 1). The dredging
zone in the Elbe River (53°32' N 9°56' E) features a depth of 13 metres and the sediment can
be characterised as muddy sand (Table 1).
For this study nine representative samples, based on significant differences regarding their
bacterial community structure were chosen (Störmer et al 2012) (Fig. 1). Eight samples were
obtained from dumping site and reference, which is located 12 kilometres north off the
dumping site. Moreover, one sample was taken in the dredging zone in the Elbe River (Fig.
1). Sampling took place in August 2009. A last dumping activity was executed in October
2008. All sediment samples were taken with a van Veen grab (0.1 m³). Onboard the sediment
was filled into a clean metal box and homogenised. For coherent analyses the samples for
analyses of the bacterial communities as well as the samples for physicochemical analyses
were taken from the same sediment. For the analysis of bacterial communities three
subsamples were stored immediately after sampling at -20°C in 50 ml falcon tubes.
All environmental data were provided by the HPA (Störmer et al 2012). The total fraction of
the sediment was analysed following the HABAK guidelines (BfG 1999).
DNA-Extraction, amplification and labelling
For DNA-Extraction the PowerSoil Kit (MoBio Laboratories, Carlsbad, CA, USA) was used
following the manufactures protocol. Three subsamples of 0.25 g sediment were collected,
and the extracted DNA was eluted in 50 µl elution buffer. Genomic DNA concentrations were
measured in duplicate by photometry using the Infinite M200 (Tecan Austria GmbH, Grödig,
Austria). Amplification and labelling were performed as described in Lu and co-workers
(2012).
67
GeoChip 4.2 hybridisation and data pre-processing
Samples were analysed with GeoChip 4.2, which was updated from GeoChip 4.0 (Hazen et al
2010, Lu et al 2012) with more genes derived from fungi and soil borne pathogens. The gene
array contains 103 666 probes targeting functional genes which are assigned to several gene
categories (antibiotic resistance, bacteria phage interaction, energy process, fungi function,
carbon, nitrogen, sulphur and phosphorus cycling, metal resistance, organic contaminant
degradation, soil benefit, soil borne pathogen, stress and virulence (Table 2). Hybridisation
and scanning were performed as previously described (Lu et al 2012). Singeltons, defined as
positive probes detected solely in one of the subsamples, were removed prior to statistical
analyses in order to remove noise from the data set. All procedures were performed by
Glomics Inc. (Norman, Oklahoma, USA).
Statistical analysis
Univariate statistics
Differences in the relative abundance of functional genes (percentage) among samples were
tested using one-way analysis of variance (ANOVA, Statistica Version 7.1, StatSoft GmbH,
Hamburg, Germany) for individual gene categories. For ANOVA tests the calculated
percentage of functional genes were arcsin-square-root transformed and a significance level of
p < 0.05 was applied. Pairwise comparisons of the samples were tested in post hoc Tukey
HSD tests (p < 0.05).
environmental variables were performed with Spearman´s rank correlation (p < 0.05).
Hierarchical clustering
For individual gene categories cluster analyses (CLUSTER 3.0; http://www.eisenlab.org)
were performed. The data were log transformed prior to the analysis. Euclidian distance was
applied as similarity metric and as cluster method average linkage was chosen. The results
were visualised using the TREEVIEW software (http://www.eisenlab.org) (Eisen et al
1999).
Multivariate statistics
Individual gene categories were compared by using 2STAGE analysis applying the PRIMER
package (PRIMER Version 6, PRIMER-E Ltd, Lutton, UK) (Clarke and Gorley 2006). The
68
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resemblance matrices of individual gene categories were calculated applying Euclidean
distance. Spearman’s rank correlation was applied to correlate individual resemblance
matrices of the gene categories in pairwise comparisons. For cluster analysis the group
average method was applied.
The relationship between functional genes and environmental variables was investigated by
distance-based multivariate multiple regression (DISTLM). In order to perform DISTLM
gene array subsamples were converted to binary values (presence/absence) since
environmental data were recorded only once per sample from each site. Calculating the binary
table, only genes present in at least two of the subsamples were regarded as present.
Environmental variables were treated as follows: Grain size fractions, sulphur (S), nitrogen
(N), phosphorus (P), carbon (C) and heavy metals were considered as single values, for PAH,
PCB, HCH and DDX single compounds were summed-up in each category. Environmental
data were log transformed prior to the analysis. Jaccard Index was applied to calculate the
resemblance matrix for functional genes. The DISTLM model was built using stepwise
selection, adjusted R² and applying 999 permutations at a significance level of p < 0.05.
Results were visualised by using distance-based redundancy analysis (dbRDA).
Results
Geochemical description of the study sites
All parameters obtained from the total fraction of the sediments are summarised in the
supplementary material (S1). The dumping centre had highest values of the grain size
fractions 100-200 µm (33 %) and 200-630 µm (25 %). Organic pollutants, in particular
polycyclic aromatic hydrocarbons (PAH, Elbe: 1.1 mg/kg, dumping centre: 1 mg/kg),
polychlorinated biphenyls (PCB, Elbe: 9.6 mg/kg, dumping centre: 7 mg/kg) and organotin
compounds (Elbe: 123.2 µg/kg, dumping centre: 78.7 µg/kg) were highest in the Elbe River
and at the dumping centre. Contrary, concentrations of sulphur (860 mg/kg), nitrogen (491
mg/kg), carbon (0.6 mg/kg) and phosphorus (290 mg/kg) as well as heavy metals were lowest
at the dumping centre. Highest TOC (1.8 mg/kg), nitrogen (2440 mg/kg) and phosphorous
(840 mg/kg) concentrations were observed in the Elbe River. The reference site, characterised
as sandy mud had highest values of the grain size fraction 20-63 µm (reference_1: 30.9 %,
reference_2 30.5 %).
69
Overview of functional gene diversity
At first, we investigated the performance of the GeoChip 4.2 referring to gene overlap and
number of detected genes. After removing 15 644 singeltons from the data set in total 18 787
genes remained for the further analyses. Subsamples (a,b,c) were compared for their similarity
according to their gene overlap (S2). Generally, we observed high similarities (> 80 %)
among subsamples. Furthermore we looked at individual gene categories in order to get an
overview of the detected genes, also in relation to the total genes covered by the GeoChip 4.2
(Table 2). We observed the highest coverage for the gene categories: Organic remediation
(25.03 %), energy process (23.93 %) metal resistance (23.23 %), soil benefit (21.11 %),
phosphorous (20.61 %) and carbon cycling (20.35 %) (Table 2).
Table 2 Overview of total and detected probes and their percentage for individual gene categories as derived
from the GeoChip 4.2.
Gene category
Antibiotic resistance Bacteria phage
Carbon cycling
Energy process Fungi function
No. total probes
3334
No. Detected probes 698
%
20.94
1071
109
10.18
11065
2252
20.35
840
201
23.93
Gene category
Nitrogen cycling
Organic Remediation
other category Phosphorus
No. total probes
9272
%
23.23
12680
1234
9.73
17061
4270
25.03
3511
301
8.57
1349
278
20.61
Gene category
soil borne pathogen
Stress
Sulphur
Virulence
1454
260
17.88
21597
3825
17.71
7101
775
10.91
3738
678
18.14
Metal resistance
soil benefit
No. total probes
3870
%
21.11
4557
911
19.99
Diversity of functional genes for individual gene categories
Diversity of functional genes was estimated by the percentage of detected genes for individual
gene categories at the different sampling sites. The sampling sites were tested for significant
differences by analysis of variance (ANOVA). Furthermore post hoc Tukey tests were applied
for pairwise comparisons of the sampling sites (S3). Detailed tables for individual gene
categories are provided within the supplemental material. Generally, the Elbe River had the
significantly highest diversity of genes regarding all individual gene categories (S3, S4). The
genetic diversity of the dumping centre was significantly lower when compared to reference
site and Elbe River.
70
CHAPTER III
___________________________________________________________________________
20
18
16
% of total genes
14
12
10
8
6
4
2
du
El
be
El a
be
m
p
du ing El b
m c be
d u p in e n tr c
m gc e
pi en a
ng t
ce er b
n
1 . tr e
5 c
k
1. m
5 a
k
1. m
5 b
2 km
km c
2 _1
km a
2 _1
km b
2 _1
km c
2 _2
km a
2 _2
km b
3 _2
km c
3 _1
km a
3 _1
km b
3 _1
km c
3 _2
km a
_
re 3 k 2 b
fe m
re _ 2
re n c c
fe e
r
_
re e n c 1 a
fe e
_
r
re e n 1 b
fe c e
re _ 1
re n c c
fe e
r
_
re e n c 2 a
fe e
re _ 2
nc b
e_
2
c
0
Fig. 2 Bar chart displaying the relative abundance of genes belonging to the gene category organic remediation
in the different samples.
Exemplarily the distribution of functional genes involved in organic remediation is depicted
in Figure 2. For each sample the percentage of detected functional genes in the three
subsamples (a,b,c) is displayed. ANOVA and post hoc Tukey test indicated significant
differences comparing the samples (p < 0.05, S3). Regarding organic remediation the Elbe
River had significantly highest functional gene diversity comparing all samples. The dumping
centre revealed significantly lower functional gene diversity compared to all samples except
1.5 km and 3 km_2 (Fig. 2, S3).
71
Hierarchical clustering of individual gene categories
Fig. 3 2STAGE analysis of similarity matrices for all gene categories. Similarities were analysed in pairwise
comparisons
The sites were further compared using hierarchical clustering. We observed highly congruent
pattern for all individual gene categories. Exemplarily, the cluster analysis for the gene
category organic remediation is shown in Figure 4. 2STAGE analysis was utilised to compare
individual gene categories in pairwise tests in order to elucidate congruency of patterns.
Consistent with the results obtained from the individual hierarchical clustering, 2STAGE
analysis indicated high similarities (rs > 0.8) among individual gene categories (Fig. 3).
Concerning the comparison of sites, each hierarchical clustering persistently displayed three
cluster groups: I) samples from the Elbe River, II) samples from the dumping centre and part
of the surrounding (1.5km, 2km_1, 2km_2, 3km_2) III) samples from the reference site and
3km_1.
72
CHAPTER III
___________________________________________________________________________
Fig. 4 Hierarchical clustering analysis of organic remediation genes based on hybridization signals using
Euclidean distance. The figure was generated using CLUSTER and visualized with TREEVIEW. White
represents no hybridization above background level and red represents positive hybridization. 1: Elbe River, 2:
dumping centre, 3: 1.5 km, 4: 2 km_1, 5: 3 km_2, 6: 3 km_1, 7: reference_2, 8: reference_1, 9: 2km_2; I)
samples from the Elbe River II) samples from dumping centre and surrounding (1.5km, 2km_1, 2km_2, 3km_2)
III) samples from the reference site and 3km_1. a) genes which were detected in all samples b) genes which were
detected only in the “Elbe” group, c) genes which were detected in the “dumping centre” group and d) genes
which were detected in the “reference” group.
73
Concerning the clustering of genes, in general four patterns were observed for all gene
categories (Fig. 4): a) genes which were detected in all samples b) genes which were detected
only in the “Elbe” group, c) genes which were detected in the “dumping centre” group and d)
genes which were detected in the “reference” group. Indeed, we did not observe differences
regarding functional genes within the different pattern. However, we observed that genes in
group I) were predominantly derived from Betaproteobacteria, while the other groups
contained genes from Delta- and Gammaproteobacteria (data not shown).
Relation of environmental factors and functional genes
The relationship between functional genes and environmental factors was investigated by a
distance-based multiple regression model (DISTLM). The influence of the dumping activity
was estimated by comparing dumping and reference sites. The Spearman’s rank correlation of
environmental variables revealed significant correlations among the fine grain size fractions,
organic carbon, sulphur, phosphorus and nitrogen content and heavy metals, such as arsenic,
lead, chrome, copper, nickel and zinc. Additionally, DDX sums correlated with the sums of
HCH, PCB and organotin compounds.
The results obtained by DISTLM are depicted as distance-based redundancy analysis
(dbRDA). The first two axes of the dbRDA explained 63.4 % of the total and 67 % of fitted
variation (Fig. 5). This indicates that the plot captures most of the salient patterns in the fitted
model. Marginal and sequential tests of the DISTLM revealed solely DDX sums to have a
significant influence on the variation in functional genes (Table 3). Apart from that DDX
sums formed a strong gradient separating samples from the dumping centre and close
surrounding from samples of the reference site.
74
CHAPTER III
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Fig. 5 Distance-based redundancy analysis (dbRDA) biplot displaying bacterial community and environmental
variables. Significant (p < 0.001) environmental factors are displayed in red.
Table 3 DISTLM results for the sequential test after considering stepwise selection of environmental factors
(p < 0.05). Significant factors bold.
Variable
Pseudo-F
Sum DDX
zinc
Sum HCH
TOC
phosphorus
nitrogen
3.30
1.38
1.22
1.35
1.84
1.67
P
0.004
0.169
0.321
0.292
0.213
0.348
Proportion
of variance
0.355
0.139
0.118
0.120
0.128
0.087
75
Discussion
Ocean dumping represents a physical perturbation for ecosystems going along with a
potentially increase in contaminants and changes in the substrate matter which may in turn
influence benthic communities (OSPAR 2004). Investigations of macrozoobenthic
communities are a fundamental element in monitoring programs to assess the impact of the
dumping activity in the dumping area. Several investigations showed that macrozoobenthic
communities respond to ocean dumping with decreasing diversity and density at dumping
sites (HPA 2010, Mühlenhardt-Siegel 1981).
Our aim was to investigate the response of the marine microbenthic (in our case bacterial)
communities to disturbance caused by the dumping of river sediment. We had two main
expectations: a) a pollutant specific response (detection of functional genes involved in -for
example- metal resistance or organic remediation) and b) differences in the functional
structure of the whole community in the greater dumping area.
The GeoChip gene array was already successfully applied in several studies investigating
environmental contamination in freshwater and marine habitats as well as in soils (Liang et al
2009, Lu et al 2012, Van Nostrand et al 2009, Waldron et al 2009). In a study on stimulated
uranium bioremediation by ethanol, it could be shown by GeoChip analysis, that gene
numbers and diversity increased due to the organic enrichment (Van Nostrand et al 2009).
Investigations on the Deepwater Horizon oil spill revealed an enrichment of genes involved in
aerobic and anaerobic hydrocarbon degradation in the plume (Lu et al 2012). In contrast to
these studies, we did not detect an increase of specific functional genes related to heavy metal
resistance or organic contaminant degradation at the dumping centre. This finding was
contradictory to our expectations since the dredged and dumped sediment contained several
organic pollutants (PAHs, organotin compounds) in relatively high concentrations.
However, we observed a general reduction in functional diversity regarding all gene
categories represented by GeoChip 4.2 at the dumping centre, which reflects large differences
in the community gene pool. This finding is explained by fundamentally different
geochemical conditions at the dumping centre resulting from the dumping activity. Our
sampling campaign took place in 2009 while several dumping campaigns were already
conducted at the site since 2005. As a consequence the dredged sediment forms a three metres
high rising on the seabed (recorded by bearing). Hence, the underlying seabed is buried
permanently and was not accessed by our sampling activity. The dumping process goes along
76
CHAPTER III
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with a portioning of the introduced river sediment while passing the water column. Coarse
sand fractions sediment immediately, while fine-grain fractions can be transported by currents
up to eight kilometres until settling down on the seafloor (HPA 2005). This explains why the
rising mainly consists of sandy sediments (grain size analyses) and is consequently relatively
poor in sulphur, nitrogen, carbon and phosphorus as well as heavy metal concentrations. The
portioning process has, as a matter of fact, consequences for sediment body or attached
pollutants, organic material and organisms since different sediment fractions charge different
loadings of pollutants, organic material and organisms (Llobet-Brossa et al 1998, Olsen et al
1982, Owens et al 2005). After dumping, the newly introduced sediment layers are exposed to
the general hydrographical regime in this area. The current at the dumping site is cyclonic and
influenced by east wind forcing (Staneva et al 2009) and the discharge of the adjacent rivers
(Howarth 2001). It should be noted that the cyclonic nature of the current was the reason to
choose this area for the dumping activities, since the dumped sediment was not expected to
spread considerably on the seafloor. Nevertheless, also in this area, upper sediment layers are
constantly relocated and mixed. The complexity of this system has to be taken into account,
when interpreting the findings of the GeoChip analyses.
The majority of the former freshwater bacterial community is dispersed together with the
smaller sediment fractions and those bacteria bound in biofilms to the sand particles have to
cope with the fundamentally different marine conditions. Although the different bacterial
community composition of marine and freshwater environments is well documented in a
multitude of studies (Bowman and McCuaig 2003, Miskin et al 1999, Ravenschlag et al 2001,
Zwart et al 2002), to the best of our knowledge no valid information exists which freshwater
bacteria survive/adapt to the marine environment or coexist in both environments on the
community level (not single species).
From our previous findings it can be emphasised that a least some freshwater bacteria
(Rhizobiales,
Hypomicrobium
and
Methylocystaceae
or
Burkholeriales
and
Hydrogenophilaceae) were still present even after 10 months exposure to the marine
environment (Störmer et al 2012). Due to the low genetic diversity (richness) detected at the
dumping centre, we emphasise, that, even after 10 months, the sediment is still in a process of
physico-chemical equilibration also concerning the bacterial community, colonisation and
differentiation. Furthermore, it can be assumed, that colonisation is further hampered by the
sediment structure itself, since coarse sands are in general less colonised by bacteria since
they offer less volume-specific surface area (Yamamoto and Lopez 1985).
77
In contrast to the dumping centre, the dumping surrounding was not covered by a thick layer
of dredged sediment. Hence, samples from the surrounding, taken by the vanVeen grab
consisted of dredged sediment as well as of the “original” marine sediment and thus were
different regarding the sediment composition compared to that of the dumping centre. This
condition supports our theory of the sediment partitioning process during dumping (see
above). Interestingly some of the samples (3km_2) from the surrounding display the same low
genetic diversity as the dumping centre clustering together regarding all gene categories
(Fig. 4). Other samples from the surrounding cluster together with the reference site
(3km_1, Fig .4).
As already mentioned the hydrographical regime at the larger dumping area is cyclonic and
influenced by east wind forcing and the discharge of the adjacent rivers. All sampling sites
where defined at the beginning of the monitoring campaigns by the HPA (HPA 2005) and
assigned to a priori areas (Fig. 1) with regard to distance to the dumping centre following a
circular design. Since this grouping solely based on the distance to the dumping centre it is
static and obviously not taking current driven relocation of sediments as well as different
environmental conditions into account.
Hence, we used multi-linear regression models (DISTLM) to estimate which factors actually
influence the functional structure of the bacterial community (Fig. 5, Table 3). In dbRDA two
sites from the close surrounding (1.5km and 2km_1) grouped together with the dumping
centre and were nicely separated from the reference sites. Interestingly, the sample 3km_2,
clustering together with the dumping centre regarding hierarchical clustering does not cluster
with the dumping centre in the DISTLM approach. This finding suggests that the low genetic
diversity at these sites is driven by different environmental factors.
The only significant explanatory variable in DISTLM was ΣDDX. Several studies
investigated the relationship between functional gene structure and environmental factors in
multivariate analyses. These studies claim that functional genes are highly correlated to
environmental factors (Waldron et al 2009, Xie et al 2011). Beforehand we tested our
variables for correlation and observed significant correlations between fine-grained sediment
fractions and various other factors such as nitrogen or carbon content and heavy metals as
well as correlations between organic pollutants. These correlations hinder an accurate
prediction of which factors influence the functional gene structure in particular. Therefore, the
significant effect of ΣDDX includes due to the high correlations ΣHCHs, ΣPCBs and
78
CHAPTER III
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Σorganotin compounds. A possible approach to disentangle these combined affects might be
the combination of controlled laboratory experiments, manipulating single factors, with field
studies. Furthermore one might consider obtaining additional, physicochemical parameters,
such as temperature, pH, oxygen penetration or redox potentials in order to additionally
estimate the bioavailability of pollutants for bacterial communities in future studies.
The results obtained from our DISTLM model suggest that ΣDDX together with the organic
pollutants ΣHCH, ΣPCB and Σorganotin, form statistically a gradient, separating dumping
and reference sites. However, our GeoChip analyses did not confirm this finding since we did
not detect any positive functional response (presence of specific organic remediation genes) at
the dumping centre observing the gene category “organic remediation”. As observed for all
other gene categories we detected less functional genes compared to the reference sites.
Beside the observed reduced functional diversity we made two other observations from
hierarchical cluster analyses: The samples clustered generally for individual gene categories
in the same manner, forming three distinct groups. However, phylogenetic differences could
be observed. A considerable number of probes clustering in group I) were retrieved from
Betaproteobacteria, while the other two groups contained probes from Delta- and
Gammaproteobacteria (data not shown). Betaproteobacteria represent typical freshwater
organisms (Miskin et al 1999, Zwart et al 2002) while Delta- and Gammaproteobacteria are
predominantly found in marine sediments (Bowman and McCuaig 2003, Bowman et al 2005,
Ravenschlag et al 1999). This observation is not surprising since it reflects the origin of the
sediment. Group I), comprising samples from the Elbe representing a freshwater habitat.
While the other groups included marine samples. Indeed this finding is in line with our results
obtained from ribosomal tag sequencing in the framework of another study, where we
subjected the same samples to a sequencing analysis. We found that community composition
of Elbe and marine stations differed significantly predominantly regarding Beta- and
Deltaproteobacteria (Störmer et al 2012).
The GeoChip 4.2 contains an impressive number of gene probes covering several functional
processes including heavy metal resistance and organic remediation. However, in our study
no differences regarding pollutant specific genes were detected when comparing dumping and
reference sites. Possibly, the pollutant load was not severe enough and a functional adaptation
did not occur. However, to date many functional processes and relationships among bacterial
communities are still not understood (Fuhrman 2009). Nowadays microbiologists face a wide
79
range of molecular tools describing microbial community function and structure.
Metagenomics, including here presented functional gene arrays, represent todays high-end
technologies offering new insights into complex microbial networks (Fuhrman 2009). They
allow for the assessment of complex systems as the bacterial response to phytoplankton
blooms (Teeling et al 2012) or the description of the rare biosphere for instance in deep sea
waters (Sogin et al 2006). Novel insights derived from studies like these will in turn improve
out methodologies. In respect to the present study additional knowledge on the function of
microbial community will lead to a further development of functional gene array as already
happened in the past years (He et al 2007, He et al 2010, Lu et al 2012).
In summary our study presented novel insights into the functional response of bacterial
communities to dumping activities. For the first time it was demonstrated that ocean dumping
leads to a reduced functional diversity at the immediate dumping centre. This study
contributed significantly to our understanding of ecosystem functioning and therefore further
progression of metagenomic technologies.
Acknowledgements
This project was funded by the Hamburg Port Authority (HPA), Bundesanstalt für
Gewässerkunde (BfG), Landesamt für Landwirtschaft, Umwelt und ländliche Räume des
Landes Schleswig-Holstein (LLUR) and Nds. Landesbetrieb für Wasserwirtschaft, Küstenund Naturschutz (NLWKN). We thank our project partners for financial and data support and
for critical discussion of the results in this study.
80
GENERAL DISCUSSION
___________________________________________________________________________
GENERAL DISCUSSION
Studying the abundance and distribution of species and factors influencing them are crucial to
understand ecosystem functioning and to predict environmental changes. Bacterial
communities are highly diverse and their biogeography depends most likely on specific
habitat conditions (Fuhrman et al 2006, Hewson et al 2007). Based on existing literature it
appears obvious that no general rules predicting the abundance or distribution of bacterial
communities exist. Principally, the combination of various environmental factors and their
characteristics determine bacterial communities in individual habitats (Fuhrman et al 2006).
Current research aims to improve our understanding of ecosystem functioning (e.g. linking
species data to environmental data) and -more importantly- to estimate or predict the
influence of environmental changes (modelling approaches). Ecosystem modelling in turn
requires the understanding of key processes in the respective environment. Coastal regions are
highly productive (Atlas and Bartha 1987) and additionally heavily impacted by
anthropogenic interferences (Lotze 2010). For these reasons modelling coastal environments
is of great interest in order to estimate or even predict the impact of anthropogenic stress
(Halpern et al 2008). Bacterial communities in coastal areas play a major role in essential
mineralisation processes and are characterised worldwide (Allan and Froneman 2008, Crump
et al 1999, Pernthaler et al 2002, Uthicke and McGuire 2007). Studies conducted on bacterial
communities aim to investigate their ecological role in various nutrient cycles; examine the
influence of environmental gradients such as salinity (Bouvier and del Giorgio 2002,
Fortunato and Crump 2011, Herlemann et al 2011) or temperature as well as contaminant
input (Paisse et al 2008). Currently, a main issue in microbial ecology represents the
understanding of spatial and temporal dynamics of bacterial communities. To date most
research concentrates on pelagic bacterial communities. Incomprehensively, knowledge on
benthic bacteria in the sublittoral shelf sediments of the German Bight remains mainly scarce.
Some studies investigated bacterial community structure and composition in the Wadden Seas
(Buhring et al 2006, Llobet-Brossa et al 1998, Musat et al 2006) or sub- and intertidal flats
(Boer et al 2009, Musat et al 2006). To our knowledge the only study addressing spatial and
temporal variations of benthic bacterial communities in the North Sea was investigating their
productivity (Duyl and Kop 1994). Information about benthic bacterial community response
to anthropogenic impacts in the German Bight does not exist. The purpose of this thesis was
to give detailed insights into community structure and diversity of benthic bacterial
communities in the German Bight. The determination of environmental factors, influencing
81
their distribution and composition was another important goal. In the discussion section the
following issues will be discussed in a general context: I) Spatiotemporal gradients
influencing benthic bacterial communities in near and offshore regions in the German Bight
II) Characterisation of benthic bacterial communities at a dumping site: investigating bacterial
community structure and function
Spatiotemporal gradients influencing benthic bacterial communities in near and
offshore regions in the German Bight
Spatiotemporal variations within bacterial communities represent a major issue in microbial
ecology (Fuhrman et al 2006, Ghiglione et al 2005, Hewson and Fuhrman 2006, Murray et al
1998). Many studies aim to identify environmental factors influencing the distribution and
assembly of bacterial communities. Seasonal changes were identified to influence bacterial
communities in various ecosystems (Fuhrman et al 2006, Pietikainen et al 2005, Yannarell et
al 2003a). Generally spoken these studies demonstrated that the occurrence of bacterial
communities is predictable from environmental factors and vice versa. This finding implies
that specific bacterial groups respond to specific environmental conditions. Fuhrman and coworkers (2006) showed that bacterial communities in the open ocean are annually
reoccurring, while bacterial communities in lake systems follow a seasonal cycle but differ
from year to year and were rather decoupled from environmental parameters (Yannarell et al
2003a). Lozupone and Knight (2007) on the other hand demonstrated for different ecosystems
that salinity variations represent the main driving force shaping bacterial community
assemblage. Summarising these efforts it becomes obvious that probably locally unique
properties of these systems are responsible for these different observations.
To date only a handful of studies exist which take into account both, spatial and temporal
dynamics of bacterial communities (Fortunato and Crump 2011, Fortunato et al 2012,
Herlemann et al 2011, Selje and Simon 2003, Selje et al 2005). Studies investigating pelagic
bacterial communities in coastal areas, more precisely estuaries, stated that spatial factors,
such as salinity and depth overwhelmed temporal factors (Fortunato et al 2012, Selje and
Simon 2003). Incomprehensively, spatiotemporal dynamics of benthic bacterial communities
in coastal regions remain little studied. The importance of seasonal variations on the structure
and productivity of marine benthic bacterial communities in the North Sea, however, was
already highlighted (Boer et al 2009, Duyl and Kop 1994). The results yielded in the course
of this thesis in conjunction with existing knowledge lead to the assumption that spatial and
82
GENERAL DISCUSSION
___________________________________________________________________________
temporal factors are from different relevance for pelagic and benthic bacterial communities as
well as for near and offshore habitats.
Our observations demonstrated that temperature effects shaped the benthic bacterial
communities in the first place while spatial factors such as salinity or grain size gradients
influenced them secondarily. Apparently, spatial variations of physicochemical factors, such
as salinity, are predominantly influencing pelagic bacterial communities in coastal regions;
contrary temporal factors are from major importance for their benthic counterparts. A possible
explanation for this finding might be the different impact of physicochemical factors on
pelagic and benthic habitats. Salinity gradients, for instance, imply density gradients which
separate water masses and thus residential bacterial communities (Fortunato et al 2012). This
impact is possibly less pronounced in sediments. Instead temporal fluctuations as
mineralisation processes after phytoplankton blooms might be, especially in highly productive
areas as coastal ones, of greater importance for benthic bacterial communities. The results
obtained in this chapter of the thesis indicated a significant impact of chlorophyll a
concentrations on the diversity and structure of benthic bacterial communities. Bentho-pelagic
coupling is a well known process in marine habitats (Buchanan 1993, Kirby et al 2007,
Marcus and Boero 1998). But only some studies investigated the linkage between organic
matter input and benthic bacterial communities. However, it was shown that organic material
sinking to the seafloor determines bacterial community structure, biomass and productivity
(Franco et al 2007, Graf et al 1982).
Further, we demonstrated that bacterial communities in offshore habitats (P8 transect)
exhibited neither distinct spatial nor temporal variations regarding their community structure,
while their counterparts in nearshore habitats (Elbe and Eider transect) showed both
significant differences on spatial as well as temporal scales. We consider that nearshore and
offshore habitats are facing different impacts of physical factors. While physical forces might
have a great impact on nearshore habitats, offshore habitats are rather unaffected. This in turn
might be reflected by the bacterial communities inhabiting these regions. We assumed that the
distance to the coastline and the linked influences of physical processes such as wind forcing
or tidal influences play a crucial role determining the variation in benthic bacterial
communities. Comparing two nearshore habitats (Elbe and Eider) it became obvious that
bacterial communities in the respective regions were influenced by different spatial gradients.
Bacterial communities along the Elbe transect were spatially significant influenced by fine
sand distributions. Bacterial communities of fine sand sediments differed significantly as
83
compared to those from muddy sediments. Bacterial communities along the Eider transect
however, were significantly influenced by salinity variations. Here, communities inhabiting
marine sediments (salinity ~ 33) differed significantly to those of estuarine sediments (salinity
~ 22). Comparing physicochemical and biogeochemical conditions of both estuaries we
observed that the estuaries different regarding their most prominent environmental gradients.
Along the Elbe transect significant spatial differences in the sediment composition but not
regarding salinity variations were observed. Contrary, along the Eider transect, salinity was
varying significantly among the sampling sites and we observed a salinity gradient decreasing
towards the estuary, while the sediment composition at the individual sampling sites was
similar. This made us conclude that the benthic bacterial community is shaped by the
respective strongest spatial environmental gradient(s) in their habitat. Both parameters,
sediment composition and salinity are known to influence benthic bacterial communities
considerably. Sandy sediments are principally less colonised by bacteria than muddy
sediments since they offer less volume-specific surface area for bacteria which can be
colonised (Yamamoto and Lopez 1985). Moreover it was highlighted that the bacterial
community structure is dependent on the sediment composition (Dale 1974, DeFlaun and
Mayer 1983). The impact of salinity variations on bacterial community assembly is well
described for bacterioplankton communities in estuaries. Further, in line with our findings,
Ikenaga and co-workers (2010) reported distinct cluster of sediment bacterial communities
along a salinity gradient.
This first approach demonstrates the enormous complexity of benthic bacterial communities
in the German Bight. Future studies should address the phylogenetic composition of the
bacterial community in near and offshore regions as well as the functional capacity of these
communities to get a more comprehensive picture of the factors, influencing benthic bacterial
communities. Simultaneous investigations of pelagic and benthic bacterial communities will
yield further insights in their respective, apparently contrary responses to environmental
factors.
Impact of dumping activities on benthic bacterial communities
This thesis provides for the first time detailed insights into bacterial community response to
dumping activities in the field. Ocean dumping, as well as other anthropogenic impacts on
marine ecosystems, represents an issue of major concern. So far, investigations on higher
organisms were conducted to estimate the impact of dumping activities on marine ecosystems
84
GENERAL DISCUSSION
___________________________________________________________________________
(IMO 2000, Mühlenhardt-Siegel 1981). Most likely dumping activities resulted in a decrease
of diversity of these communities at the immediate dumping area.
In an interdisciplinary project bacterial community analyses were realised at a dumping site in
the German Bight. Bacterial communities of the dumping and a reference site were analysed
and compared to estimate the impact of the dumping activity on the bacterial community. The
dumping activity resulted in changes of the substrate matter at the immediate dumping site
(HPA 2010). The dumping site consisted of sandy material while the reference region was
characterised by sandy mud. This difference was mirrored in the bacterial community
structure. Bacterial communities from dumping and reference sites differed significantly
regarding their community structure. The steep grain size gradient appeared to be the
strongest environmental gradient affecting significantly the bacterial community in this
region. Obviously, the intrusion of this sediment represented a massive perturbation for the
environment. This was shown when bacterial communities at the immediate dumping site
were compared before and after a dumping activity. Before a dumping event bacterial
community structures obtained at several sampling sites (centre and close surrounding) at the
immediate dumping site were rather. After dumping, however, significant differences were
observed when communities of the immediate dumping centre were compared to those of
rather external sampling sites at the dumping site. The impact of perturbation events was
already investigated in various contexts. Principally, changes in the bacterial community
structure were reported (dos Santos et al 2011, Edlund and Jansson 2006, Edlund et al 2006,
Findlay et al 1990). In the present case multivariate analyses identified not only grain size
distributions but also -to a lower extent- organic pollutants to be the main driving forces in
shaping bacterial community structure in the investigated dumping area. The impact of
organic pollutants was, due to high correlations among environmental variables, delicate to
assess. Significant effects of organotin compounds as revealed in all redundancy analyses for
instance, are predominantly a statistical artefact. Organotin compounds are highly correlated
to other organic pollutants such as poly cyclic aromatic hydrocarbons, HCHs or PCBs. These
correlations hinder a precise assessment of individual effects on the benthic bacterial
community. Most of field studies face the problematic of correlations among pollutants with
other environmental variables (Dean-Ross and Mills 1989, Gillan et al 2005). Moreover, since
sufficient information about physicochemical parameters such as oxygen penetration and pH
are missing, the bioavailability of these compounds is questionable. To further elucidate the
individual impact of pollutants on benthic bacterial communities controlled laboratory studies
85
need to be conducted. These studies should approach the disentangling of individual effects
by manipulating single environmental factors (e.g. decoupling of grain size and pollutants).
Along with the freshwater sediment freshwater bacteria entered the dumping site and were
still detectable ten months after the dumping activity. Rhizobiales, Hypomicrobium and
Methylocystaceae or Burkholeriales and Hydrogenophilaceae seem to successfully establish
at the dumping centre. Together with the observation of considerably higher numbers of
Desulfuromonadaceae and Flavobacteriaceae these findings point to a formation of a
specialised bacterial community at the dumping centre as a consequence of the dumping
activity. To our knowledge, the establishment of bacterial freshwater communities in marine
waters is little studied. The abrupt intrusion of freshwater communities into marine systems is
naturally rather untypical. The marine-freshwater boundary represents under natural
conditions a difficult barrier to cross and marine and freshwater phylotypes are believed to be
clearly evolutionary separated (Logares et al 2009). Our results demonstrate, however, that
certain freshwater bacteria were still detectable ten months after the dumping activity,
suggesting that these groups successfully established under marine conditions. Experimental
studies could potentially provide further insight in the possible cross-colonisation of these two
environments by testing physicochemical and ecological conditions (Logares et al 2009).
We demonstrated that the dumping activity affected bacterial community structure and
diversity at the dumping site. To further elucidate the impact of the ocean dumping we aimed
to investigate to which extent the functional diversity of the bacterial communities at the
dumping site differs compared to those of a previously defined undisturbed reference site
(HPA 2005) and those communities of the dredging zone in the Elbe River. To do so
functional gene arrays were implemented to gain information about the functional structure of
the bacterial communities. The applied gene array, GeoChip, was already utilised in various
other environmental studies (He et al 2010, Lu et al 2012, Van Nostrand et al 2009, Xie et al
2011). The GeoChip 4.2 contains 103 666 probes of functional processes such as: antibiotic
resistance, bacteria phage interaction, energy process, fungi function, carbon, nitrogen,
sulphur and phosphorus cycling, metal resistance, organic contaminant degradation, soil
benefit, soil borne pathogen, stress and virulence. For all these categories a significant lower
functional diversity for the bacterial community at the dumping centre as compared to the
reference site was observed. Hence, we suggest that the dumping activity led most likely to a
reduction of the overall gene inventory at the dumping site. As already discussed in the
previous section, due to the dumping activity fundamentally different geochemical conditions
86
GENERAL DISCUSSION
___________________________________________________________________________
at the dumping site were created. The sandy, regarding sulphur, nitrogen and carbon content
poor material harboured a less diverse bacterial community as compared to the reference. The
low diversity of the bacterial community might in turn explain the lower functional diversity
at the dumping site. The presence of few bacterial metabolic types implies also a lower
functional diversity. To date concrete investigations linking bacterial community diversity and
functional diversity are lacking. One might argue that the observed lower functional diversity
represents only an artefact of the GeoChip analysis. Possibly, functional genes are not covered
by the array because they are not yet discovered. Undisputable many functional processes and
relationships among bacterial communities are still not understood (Fuhrman, 2009).
However, comparing the functional diversity of the bacterial communities at the dumping site
to those of the reference it is valid to state that the diversity of investigated functional genes is
significantly lower and most likely a result from the dumping activity.
Beside the reduced functional diversity of bacterial communities at the dumping site,
hierarchical clustering of the samples showed similar distinct cluster for all individual gene
categories. In all cases, samples originating from the Elbe River, dumping centre and
reference site formed separate cluster. Interestingly, the clustering based not on different
functional genes but on different phylotypes from which these genes were derived.
Principally, the Elbe River cluster contained genes derived predominantly from freshwater
bacteria, contrary mainly genes from marine phylotypes were detected in the reference group.
The dumping site group however contained genes derived from both freshwater and marine
bacteria. We assume that the bacterial community at the dumping site comprises a consortium
of marine and fresh water phylotypes and that some marine functions may be replaced or in
parallel executed by freshwater counter parts. The investigations of our sequencing approach
are confirming this assumption since we detected freshwater and marine phylotypes at the
dumping centre.
Since both approaches, sequencing and functional gene array base on DNA, no information
about metabolically active bacterial communities is given. It might be considered to integrate
further molecular approaches basing on RNA (Transcriptomics) or even proteins (Proteomics)
to yield sufficient information about whether the detected freshwater groups are still
metabolically active. Metagenomics, including (Meta)transcriptomics and Meta(proteomics),
represent today’s high-end technologies offering new insights into complex microbial
networks (Fuhrman 2009). They allow for the assessment of complex systems as the bacterial
87
response to phytoplankton blooms (Teeling et al 2012) or the description of the rare biosphere
for instance in deep sea waters (Sogin et al 2006).
Conclusion
The outcome of this thesis significantly broadened our knowledge and understanding of
benthic bacterial communities in the German Bight. Although bacterial community structures
were highly variable; we were able to determine environmental factors influencing the
bacterial community structure and diversity.
It was highlighted that the distance to the coast and implicated differences in the impact of
physical factors and hydrographics form distinct regional regimes (offshore vs. nearshore).
The amplitude of physicochemical and biogeochemical gradients in these regions was
differently pronounced. In general, offshore regions were characterised by rather stable
physicochemical and geochemical conditions and benthic bacterial communities rather
disperse showing neither spatial nor temporal variations. In contrast the observed nearshore
regions exhibited significant variations regarding physicochemical (namely salinity and
temperature) and biogeochemical (grain size) parameters. Benthic bacterial communities
varied significantly on both spatial and temporal scales. Temperature was considered to play
the dominant role in shaping the bacterial communities in both nearshore regions. Spatially
sediment composition and salinity were shown to influence the bacterial community structure
whereas the respective strongest environmental gradient dominated. We therefore conclude
that to understand the distribution and abundance of benthic bacterial communities the
amplitude of physicochemical gradients and the impact of physical forces and hydrodynamics
is most important and needs to be considered.
The dumping activity of lightly polluted sediment in the German Bight resulted in a
fundamentally change of substrate matter at the immediate dumping site. The steep
environmental gradient formed by grain size distribution significantly affected bacterial
community structure and diversity as well as the functional diversity. Community and
functional diversity of the bacterial community were significantly lower when compared to a
reference site. Moreover we demonstrated that freshwater phylotypes were still detectable ten
months after the dumping activity. The effect of pollutants however, was due to high
correlations amongst each other delicate to assess. Remarkably higher numbers of
Flavobacteriaceae and Desulforomonadaceae might be an indication for organic pollution at
the dumping centre since both families were already named in this context. We therefore
88
GENERAL DISCUSSION
___________________________________________________________________________
conclude that the dumping activity led to a specific environment inhabited by a adapted
bacterial community. The impact of the dumping activity, however, was localised solely at the
immediate dumping site.
This thesis comprises the most detailed investigations of benthic bacterial communities in the
German Bight. Important knowledge on bacterial community structure and influencing
environmental factors was presented. The insights gained by these investigations are crucial
for our understanding of ecological process and anthropogenic impacts in coastal areas. We
are convinced that the perceptions yielded by this will help estimating and predicting
environmental changes in the German Bight.
89
SUMMARY
Bacterial communities are highly diverse and their composition and distribution depends most
likely on individual habitat conditions. Hence, studying the abundance and distribution of
species and factors influencing them are crucial to understand ecosystem functioning and to
predict environmental changes. This thesis aimed to characterise benthic bacterial
communities and environmental factors influencing them in the German Bight. The German
Bight represents a highly variable and human-impacted system and to date only little is
known about the respective consequences for benthic bacterial communities.
The biogeography of benthic bacterial communities in the southern German Bight was
captured in monthly cruises along three transects obtaining simultaneously physicochemical
and biogeochemical parameters. Ocean dumping activities performed in the German Bight
represent a topic of actual concern and their impact on benthic bacterial communities was not
included in regular monitoring programs so far. In a pilot study community analyses were
implemented at an active disposal site for dredged sediments. Differences in the bacterial
community structure and diversity were estimated in direct comparison to a reference site.
Applying ARISA fingerprinting community structure and diversity of benthic bacteria were
assessed. Sequencing of the SSU ribosomal DNA was implemented to determine the
community composition. And finally, functional gene array analyses were utilised to
investigate the functional structure of the bacterial communities. The bacterial community
information was linked to the recorded contextual data via multivariate analyses in order to
identify main factors shaping the community and functional structure.
Generally we observed highly diverse benthic bacterial communities. Bacterial communities
inhabiting nearshore and offshore habitats in the German Bight were differently affected by
respective environmental conditions. We demonstrated that bacterial communities in
nearshore habitats exhibited distinct temporal as well as spatial variations which were not
observed for those inhabiting offshore regions. In any case temporal influences were
determined to play the major role. The spatial variations were predominantly driven by
respective strong environmental gradients, here grain size and salinity variations, occurring in
two compared nearshore regions.
Our investigations at a disposal site demonstrated that the dumping activities affected benthic
bacterial communities. Changes in the substrate matter at the dumping site determined a
90
SUMMARY
___________________________________________________________________________
significantly different community structure and diversity of the benthic bacteria as compared
to those at a reference site. We observed a considerably lower diversity regarding the
community and functional level of the bacteria. Finally, our sequencing approach revealed
that the bacterial community at the dumping site encompasses marine as well as fresh water
phylotypes which were most likely introduced with the intrusion of dumped sediment. These
findings leads us to conclude that the dumping activity created fundamentally different habitat
conditions at the immediate dumping site and determined thereby an adapted bacterial
community.
This thesis comprises the most detailed investigations of benthic bacterial communities in the
German Bight. Important knowledge on bacterial community structure and influencing
environmental factors was presented. The insights gained by these investigations are crucial
for our understanding of ecological process and anthropogenic impacts in coastal areas. We
are convinced that the perceptions yielded by this thesis will help in estimating and predicting
environmental changes in the German Bight.
91
ZUSAMMENFASSUNG
Bakteriengemeinschaften sind sehr divers und ihre Zusammensetzung wird maßgeblich durch
die Bedingungen in ihrem jeweiligen Habitat bestimmt. Die Untersuchung von
Wechselbeziehungen zwischen Bakteriengemeinschaften und zugehörigen Umweltfaktoren
ist deshalb essentiell um die Zusammenhänge zwischen dem Vorkommen bestimmter Arten
und
äußeren
Einflüssen
zu
verstehen
und
gegebenenfalls
das
Ausmaß
von
Umweltveränderungen abschätzen zu können.
Die vorliegende Arbeit dokumentiert zum ersten Mal die Verbreitung benthischer
Bakteriengemeinschaften in Abhängigkeit einflussnehmender Umweltfaktoren in der
Deutschen Bucht (Nordsee). Die Deutsche Bucht selbst stellt eine sehr variable und durch
anthropogene Einflüsse geprägte Region dar.
Die Zusammensetzung benthischer Bakteriengemeinschaften wurde in monatlichen
Abständen entlang dreier Transekte in der Deutschen Bucht erfasst und mit gleichzeitig
erhobenen physikochemischen und biogeochemischen Daten verschnitten. Umlagerungen von
ausgebaggertem Elbsediment in die Deutsche Bucht im Zuge von Instandhaltungsarbeiten des
Hamburger Hafens sind aktuell von großem, auch öffentlichem Interesse. Bisher wurden
Gemeinschaftsanalysen
von
benthischen
Bakterien
nicht
in
das
begleitende
Monitoringprogramm integriert. In einer Pilotstudie wurden diese Analysen durchgeführt um
den Einfluss der Verbringung auf die Bakteriengemeinschaften abzuschätzen.
Bakteriengemeinschaftsanalysen (Struktur und Diversität) wurden im Rahmen dieser Arbeit
mittels der Fingerprintmethode Automated Ribosomal Intergenic Spacer Analysis (ARISA)
durchgeführt. Darüber hinaus wurde die Zusammensetzung der Bakteriengemeinschaften
mithilfe von Tiefensequenzierung einer ribosomalen DNA Sequenz ermittelt und die Funktion
mittels Mikroarrays (functional gene arrays) untersucht. In multivariaten Analysen wurden
die Informationen der Gemeinschaftsanalysen mit kontextuellen Daten verschnitten.
Die Untersuchungen ergaben, dass die benthischen Bakteriengemeinschaften der Deutschen
Bucht sehr divers sind. Der Einfluss von Umweltfaktoren auf die Bakteriengemeinschaften
hängt dabei stark von den physikalischen Rahmenbedingungen (Wind, Tide) in den
untersuchten Gebieten ab. Bakteriengemeinschaften der nahen Küstengebiete zeigten
ausgeprägte saisonale sowie räumliche Abhängigkeiten auf, während Gemeinschaften in
92
ZUSAMMENFASSUNG
___________________________________________________________________________
küstenfernen Gebieten weniger von Umweltfaktoren beeinflusst waren. In jedem Fall spielte
die Temperatur bei der Ausprägung der Bakteriengemeinschaften eine entscheidende Rolle.
Bezüglich der untersuchten Ästuare der Küstenregionen konnte gezeigt werden, dass der
jeweils am stärksten ausgeprägte Umweltgradient, in diesem Fall Unterschiede des
Salzgehaltes und des Feinsandanteils im Sediment, den größten Einfluss auf die
Bakteriengemeinschaft nahm.
Die in der Deutschen Bucht stattfindenden Sedimentumlagerungen führten zu einer
fundamentalen Veränderung der Sedimentstruktur an der Einbringstelle. Die Veränderung
spiegelte
sich
auch
in
den
vorkommenden
Bakteriengemeinschaften
wider.
Die
Gemeinschaftsstruktur unterschied sich signifikant von derer im Referenzgebiet. Die
Diversität, im Hinblick auf Funktion und Artenniveau, war ebenfalls deutlich erniedrigt. Die
Sequenzanalysen ergaben, dass neben marinen Arten auch Süßwasserbakterien an der
Umlagerungsstelle nachgewiesen wurden. Insgesamt lässt sich feststellen, dass die
Umlagerung zu einer deutlichen Veränderung der Habitatstruktur geführt hat die
konsequenterweise zu einer angepassten Bakteriengemeinschaft führte.
Insgesamt
bietet
diese
Arbeit
einen
detaillierten
Einblick
in
die
benthischen
Bakteriengemeinschaften der Deutschen Bucht. Es konnte gezeigt werden welche und in
welchem Ausmaß Umweltfaktoren diese Gemeinschaften beeinflussen und wie sich
Sedimentverbringungen im Besonderen auswirken. Die Erkenntnisse dieser Arbeit sind
entscheidend um ökologische Prozesse und Veränderungen in Küstenregionen der Deutschen
Bucht zu verstehen und abschätzen zu können.
93
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DANKSAGUNG
An erster Stelle möchte ich mich bei Dr. Antje Wichels und Dr. Gunnar Gerdts bedanken.
Ohne ihr Engagement dieses Projekt ins Leben zu rufen, hätte ich diese Arbeit wohl nicht
anfertigen können. Ich bin sehr dankbar dafür, dieses interessante und auch herausfordernde
Projekt bekommen zu haben. Eure Betreuung ist einzigartig und etwas besonderes! Ich habe
dank Euch nicht nur viel über die Mikrobiologie sondern auch über das nicht zu verachtende
„Drum-Herum“ gelernt. Vielen Dank für die tolle Unterstützung!
Bei meinen Projektpartnern, der Hamburg Port Authority (HPA), der Bundesanstalt für
Gewässerkunde (BfG), dem Landesamt für Landwirtschaft, Umwelt und ländliche Räume des
Landes Schleswig-Holstein (LLUR) und dem niedersächsischem Landesbetrieb für
Wasserwirtschaft, Küsten- und Naturschutz (NLWKN-BSt Norden-Norderney) möchte ich
mich für die Finanzierung meines Projektes und die gute Zusammenarbeit bedanken.
Besonderer Dank gilt Dr. Maja Karrasch für die zahlreichen Gespräche und Einführungen in
die Mühlen der Behörden. Für die interessanten und unkomplizierten Probenahmen im
Rahmen des Monitoring möchte ich mich stellvertretend für alle Kollegen bei Rolf Lüschow
und Uwe Hentschke bedanken. Ich habe so viel gelernt!
Mein thesis committee bestehend aus Dr. Antje Wichels, PD Dr. Sabine Kasten, Dr. Gunnar
Gerdts, Dr. Alban Ramette und Prof. Dr. Wolfgang Streit stand mir sprichwörtlich von der
ersten Minute an mit viel Engagement und konstruktiver Kritik zur Seite. Ich danke
Ihnen/Euch sehr für die Zeit, die Sie/ihr in mich und mein Projekt investiert habt und die tolle
Betreuung! Ganz besonderen Dank für die Betreuung meiner Promotion an der Universität
Hamburg möchte ich Prof. Dr. Wolfgang Streit und PD Andreas Pommerening-Röser
aussprechen, sowie Jun. Prof. Dr. Mirjam Perner und Prof. Dr. Friedrich Buchholz, die sich
bereit erklärt haben als meine Disputationsgutachter zu fungieren. Prof. Myron Peck hat die
vorliegende Arbeit als Native-Speaker begutachtet auch dafür vielen herzlichen Dank.
Die Zeit in unserer Arbeitsgruppe Mikrobielle Ökologie und das Leben an/mit der BAH
gehört wohl zu den bereicherndsten Abschnitten in meinem Leben. Ich danke meinen
Kollegen und Freunden in unserer Arbeitsgruppe für die schöne und entspannte
Arbeitsatmosphäre, die „wirkliche“ Einführung in das Leben als mirkobielle Ökologin. Ganz
besonders möchte ich mich bei Sonny, Judith, Maddin, Evamaria und Réne bedanken, die mit
mir Freude und Problematiken nicht nur im Laboralltag geteilt haben!
108
DANKSAGUNG
___________________________________________________________________________
Bei Prof. Dr. Karen Wiltshire bedanke ich mich sehr für die Bereitstellung ihrer Daten ohne
die eine Auswertung von Teilen dieser Arbeit nicht möglich gewesen wäre! Kristine, Sylvia,
Julia und der Uthörn Crew danke ich von Herzen für ihre Unterstützung bei der Probennahme
auf der wundervollen Uthörn, die Überwältigung der CHN Tücken und eine großartige Zeit
auf See.
Von allen Geschenken, die uns das Schicksal gewährt, gibt es kein größeres Gut als die
Freundschaft - keinen größeren Reichtum, keine größere Freude (Epikur von Samos). Ich
möchte mich aus tiefstem Herzen bei all meinen lieben Freunden bedanken, die mich in so
großartiger weise begleitet und unterstützt haben: Sonny du bist einfach nur „Rock’n’Roll und
mit das Größte was es auf der Welt gibt! Judith, ich bin so dankbar, dass es Dich gibt und wir
uns nach einigen Wirrungen doch nochmal wieder getroffen und uns „vertieft“ haben. Flori,
du bist der große Bruder, den ich nie hatte und immer wollte ;). Ich danke Steffi, Tommi,
Maddin und Matze für eine großartige Zeit, den Kaffee, das Bier und einfach nur den Kopf
ausschalten zu können. Ein dicker Drücker geht auch an meine „alten Freunde“ (besonders
Dani, Fabi, Igo, Jenny) die immer an mich geglaubt haben!
Zum Schluss möchte ich mich bei meiner Familie, besonders meinen Eltern und meiner
Schwester Jessica bedanken. Ihr habt mich in vielen Punkten zu dem gemacht, was ich heute
bin und besonders meine Eltern haben mich schon früh die Faszination Biologie gelehrt! Ich
bin euch sehr, sehr dankbar! Nicht nur für die finanzielle Unterstützung sondern besonders
auch für all die Nachsicht und den guten Zuspruch vor allem in den letzten Monaten.
109

Dokument 1 - E-Dissertationen der UHH

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